Project In Humanity
What if a large group of unwitting geoengineers have been implementing a global project that alters the climate and modifies the weather in a misguided and misinformed attempt to advance civilization?
Originally published: February 10, 2026. Last updated: August 17, 2026
Please watch all of the videos below:
You have been lied to for nearly two decades.
Take some time to challenge your assumptions.
https://www.youtube.com/watch?v=mS1bci-aS6c
Source Video #1: Medical Doctors For COVID Ethics, International
Source Video #2: Truth Action Project
Additional Interview: The Patriot Pulse Podcast
Please take the time to read this article in its entirety in order to comprehend the true dangers inherent in a scientific operation (Sci-Op) such as this. After you have read the complete article, please share it far and wide:
ProjectInHumanity.com
This is just the first in a series of articles.
I encourage you to read them all:
1. Seeking The Truth
2. Project In Humanity
3. What Causes The White Lines In The Sky?
4. Nearly Every Nation on Earth Agreed to a Moratorium on Geoengineering in 2010
5. The Gaping Loophole in U.S. Federal Law Regarding Weather Modification Reporting
6. Air Traffic Related Air Pollution
7. Get The Lead Out! (Deadline for comment was March 13, 2026)
8. Strontium, Aluminum and Barium, Oh My!
9. Aerotoxic Syndrome
10. The Air Quality Act
11. Petition to Stop Geoengineering
12. Missouri’s Clean Skies Act
13. Blocking the Sun with Amorphous Silica
I realize that these infographics may be difficult to read on a phone. Download the PDF in order to enlarge them for better readability.
Belief in the false chemtrail / geoengineering narrative prevents understanding of the true problem and thus it blocks real solutions.
MESSAGES TO TAKE HOME :
Every plane, every helicopter, every jet, every rocket, every missile and every piece of space junk leaves a trail of exhaust in its wake.
Pollution (not spraying) explains what is being seen in the sky.
The chemtrail / geoengineering narrative is a false flag / sci-op.
Jet engine exhaust contains toxic pollutants, not just water vapor.
Emissions from jet engine exhaust pollution, rockets and missiles at altitude in the stratosphere is essentially unintentional geoengineering.
Contrails depend on atmospheric conditions and they persist when jets travel through Ice Super Saturated Regions.
Most jet engine exhaust pollution (JEEP) is invisible ~95% of the time.
The scale of global aviation is enormous - 100 billion gallons of jet fuel are combusted during 100,000+ flights/day.
Aviation and rocketry combined are the largest weather modification/ geoengineering project in the history of mankind.
Invisible, microscopic pieces of particulate matter act as cloud condensation nuclei.
A wide range of metals are emitted in jet engine exhaust pollution.
Rocket emissions significantly contribute to pollution, emitting millions of pounds of aluminum and other toxins each year.
The aviation and rocket industries benefit from the chemtrail / geoengineering narrative and thus avoid accountability.
Jet fuel contains harmful compounds. (e.g., sulfur, aromatics, naphthalene and metals).
Pollution from aviation and rocketry slowly falls to Earth and impacts the ozone layer, weather and human health.
Clouds caused by aviation alter the temperature.
There is no evidence for spraying infrastructure.
Nanoparticle emissions are massive (350 septillion particles per year).
Contrails have been around for decades and behave the same way as they always have, there are simply many more of them due to increased air traffic.
Leaded aviation gasoline (AvGas) contributes to pollution.
Regulation focuses on visibility of exhaust and its overall mass but not the actual number of microscopic particulates.
Pollution reduction is possible but has not been implemented because the industry controls the regulatory agencies, not the other way around.
Intentional geoengineering exists but it is at a much smaller scale, mostly limited to computer modeling and small tests.
The demise of satellites and the reentry of space junk into the mesosphere adds particulate matter that contributes to the white milky haze in the sky.
Pollution, in the form of particulate matter, may suppress precipitation in certain areas, leading to drought in some areas and flooding in others.
Every flight and every launch adds to the cumulative burden in our atmosphere.
Particulate pollution is a global, persistent and long-term problem’
Solutions exist: cleaner fuels, engine redesign, filters, operational changes and real regulation.
Real solutions require truth, transparency and holding polluters accountable
Look Up. Question Everything. Demand real solutions for a livable future.
The pollutants listed in the infographic below are a conservative estimate of the total amount of pollution released into the atmosphere every year by the aviation and rocketry industries.
Over 120 BILLION gallons of jet fuel are combusted every year globally, so multiply the numbers below by 120 MILLION
1,000 gallons of jet fuel equals ~6,677 pounds
120 BILLION gallons = ~800 BILLION pounds
Approximately 4.4 kg of CO₂ + H₂O are produced for every kilogram of jet fuel burned. The extra mass comes overwhelmingly from oxygen extracted from ambient air in the atmosphere.
Jet fuel itself contains relatively little nitrogen, but jet engines ingest enormous quantities of atmospheric N₂. High combustion temperatures cause a portion of that nitrogen to participate in combustion chemistry.
NO is generally the dominant primary NOₓ species immediately after combustion.
N₂ + O → NO + N
followed by additional reactions involving N₂, O₂ and radicals.
NO is subsequently oxidized:
2 NO + O₂ → 2 NO₂
NO₂ is therefore both a direct combustion product and an important product of subsequent plume chemistry.
N₂O can occur at trace concentrations as a combustion product.
It is substantially less abundant than NO and NO₂.
Recent synthesis of aircraft-engine measurements confirms that NOₓ increases strongly with thrust, while CO and hydrocarbons generally decrease as thrust increases.
CO is especially important at:
idle
low thrust
startup
transient operation
It is generally much less important at high thrust.
Unburned hydrocarbons
Not every hydrocarbon molecule entering the combustor is completely oxidized.
The resulting exhaust may contain:
Alkanes
methane
ethane
propane
n-butane
isobutane
pentanes
hexanes
heptanes
octanes
higher molecular-weight alkanes
Alkenes
ethylene
propylene
butenes
butadienes
Alkynes
acetylene
Cycloalkanes
cyclopentane derivatives
cyclohexane derivatives
substituted cycloalkanes
Aromatic hydrocarbons
benzene
toluene
ethylbenzene
xylenes
trimethylbenzenes
styrene
naphthalene
substituted naphthalenes
Aircraft-exhaust studies have identified numerous speciated hydrocarbons, including n-hexane, benzene, toluene, ethylbenzene, xylene, styrene, 1,3-butadiene and aromatic compounds.
Oxygenated organic compounds
Incomplete combustion and subsequent atmospheric oxidation generate numerous oxygen-containing organic compounds.
Aldehydes
formaldehyde — HCHO
acetaldehyde — CH₃CHO
propionaldehyde/propanal — C₂H₅CHO
acrolein — CH₂=CHCHO
benzaldehyde
butyraldehyde and higher aldehydes
Ketones
acetone
methyl ethyl ketone
other substituted ketones
Organic acids
formic acid
acetic acid
propionic acid
other low-molecular-weight carboxylic acids
Phenolic compounds
Potential trace products include:
phenol
cresols
substituted phenols
The FAA/EPA-oriented aircraft exhaust literature specifically identifies formaldehyde, acetaldehyde, acrolein and propionaldehyde among aircraft exhaust pollutants.
Polycyclic aromatic hydrocarbons and related compounds
High-temperature combustion and soot formation can produce polycyclic aromatic hydrocarbons (PAHs).
naphthalene
acenaphthylene
acenaphthene
fluorene
phenanthrene
anthracene
fluoranthene
pyrene
benz[a]anthracene
chrysene
benzo[b]fluoranthene
benzo[k]fluoranthene
benzo[a]pyrene
indeno[1,2,3-cd]pyrene
dibenz[a,h]anthracene
benzo[ghi]perylene
The exact PAH distribution varies greatly with engine operating condition and combustion efficiency.
PAHs may occur in both:
the gas phase, and
particulate/soot-associated material.
Particulate matter
Aircraft exhaust contains particles spanning a very wide size range.
Nonvolatile particulate matter — nvPM
The principal primary carbonaceous particulate material includes:
elemental carbon
soot
black carbon
organic carbon
condensed hydrocarbons
ash
trace metals
sulfate-associated material
ICAO specifically regulates aircraft-engine nonvolatile particulate matter in terms of both mass and particle number.
Soot
Soot is predominantly carbonaceous material formed through high-temperature hydrocarbon chemistry.
It contains:
elemental carbon
organic carbon
condensed hydrocarbons
PAHs
trace inorganic material
Soot particles can subsequently acquire coatings of:
sulfuric acid
sulfate
water
organic compounds
nitrate
other secondary atmospheric products.
Ultrafine particles
Aircraft combustion generates enormous numbers of particles in the nanometer-to-ultrafine range.
Particle number and particle mass are very different quantities: an exhaust plume can contain enormous numbers of ultrafine particles while their total mass remains relatively small.
Metals and inorganic elements
This is an especially important category because metals in aircraft exhaust can have several different origins.
They can originate from:
trace constituents naturally present in petroleum;
fuel additives;
lubricating oils;
engine materials;
corrosion;
mechanical wear;
contamination during refining, storage or transportation.
Aircraft-exhaust studies have detected numerous elements in particulate emissions. A reported elemental suite included:
magnesium — Mg
silicon — Si
phosphorus — P
sulfur — S
chlorine — Cl
potassium — K
calcium — Ca
titanium — Ti
chromium — Cr
manganese — Mn
iron — Fe
nickel — Ni
copper — Cu
zinc — Zn
bromine — Br
silver — Ag
indium — In
antimony — Sb
tellurium — Te
iodine — I
thallium — Tl
The same study found total measured elemental emissions of approximately 6.3–27.5 mg/kg fuel.
For 3,028 kg fuel:
6.3 mg/kg × 3,028 = 19.1 g
27.5 mg/kg × 3,028 = 83.3 g
Therefore, the reported range corresponds to approximately:
19–83 g of measured elemental particulate material per 1,000 gallons
This is an extremely important qualification: these numbers do not mean that 19–83 g of each element is emitted. They represent the combined mass of the measured elemental species.
Petroleum-derived trace metals
Petroleum can naturally contain trace metals, although their concentrations in finished aviation fuel are generally very small and are controlled indirectly by refining and fuel specifications.
Potential petroleum-derived metals include:
vanadium — V
nickel — Ni
iron — Fe
copper — Cu
zinc — Zn
sodium — Na
calcium — Ca
magnesium — Mg
potassium — K
chromium — Cr
manganese — Mn
cobalt — Co
lead — Pb
arsenic — As
cadmium — Cd
mercury — Hg
selenium — Se
antimony — Sb
tin — Sn
However, presence in petroleum does not mean that all of these elements occur at significant concentrations in every Jet A/Jet A-1 fuel.
Nickel and vanadium are particularly characteristic trace metals of crude petroleum and petroleum residues, whereas Fe, Cu and Zn can also enter aviation fuel through refining equipment, storage and transportation.
The aircraft-exhaust literature specifically identifies trace Fe, Cu and Zn in fuel as contributors to exhaust by-products.
Fuel-additive-derived exhaust species
Jet fuel can contain a number of approved additives. Importantly, not every aircraft fuel contains every additive.
The principal additive categories include:
antioxidants
metal deactivators
static dissipators
fuel-system icing inhibitors
corrosion inhibitors
lubricity improvers
biocides
thermal-stability additives
leak-detection additives
The particular package depends on the fuel specification, refinery treatment, purchaser requirements and military/civilian application.
Antioxidants
Approved aviation-fuel antioxidants include hindered phenols such as:
2,6-di-tert-butylphenol
2,6-di-tert-butyl-4-methylphenol
2,4-dimethyl-6-tert-butylphenol
related alkylated phenols
These compounds are normally present at only tens of mg/L or less.
For example, an ASTM-listed antioxidant concentration can be as high as approximately 24 mg/L.
At 24 mg/L:
3,785 L × 24 mg/L = 90.8 g additive
Thus, the absolute quantity of antioxidant in 1,000 gallons can be on the order of tens of grams.
During combustion, these molecules are primarily oxidized to:
CO₂
H₂O
but incomplete combustion can produce trace:
CO
aldehydes
phenols
aromatic hydrocarbons
PAHs
soot/organic particulate matter
Metal deactivators
A commonly approved metal deactivator is:
N,N′-disalicylidene-1,2-propanediamine
It is used to complex trace metals such as copper and thereby reduce their catalytic effects on fuel oxidation.
Approved concentrations are very small. One specification gives an initial maximum of approximately 2 mg/L, with cumulative redoping up to approximately 5.7 mg/L.
At 2 mg/L:
3,785 × 2 mg = 7.57 g
At 5.7 mg/L:
3,785 × 5.7 mg = 21.6 g
Combustion products can include:
CO₂
H₂O
CO
NOₓ
aromatic/organic fragments
trace particulate-bound carbon
The nitrogen atoms in the additive provide an additional potential nitrogen-containing combustion source, although the amount is tiny compared with atmospheric N₂ entering the engine.
Static-dissipator additives
Stadis 450 is widely used in aviation fuel.
It is a complex proprietary additive rather than a single pure compound. Its active chemistry includes dinonylnaphthylsulfonic-acid-type material, and published descriptions of the commercial formulation identify additional hydrocarbon solvents/components.
Aviation specifications permit concentrations of only a few mg/L. A common maximum is approximately 3 mg/L for initial doping, with cumulative concentrations up to approximately 5 mg/L in some specifications.
At 3 mg/L:
3,785 × 3 mg = 11.4 g additive
Potential combustion products include:
CO₂
H₂O
SO₂/SO₃
sulfate/H₂SO₄
CO
hydrocarbon fragments
aromatic compounds
soot
The sulfur-containing portion is particularly relevant because the additive itself can contain sulfur.
Fuel-system icing inhibitors
A commonly used fuel-system icing inhibitor is:
Diethylene glycol monomethyl ether (DiEGME)
Another historically used material is:
Ethylene glycol monomethyl ether (EGME)
Typical concentrations are approximately 0.10–0.15% by volume for the relevant additive.
At 0.15% of 3,785 L:
~5.68 L additive
Depending on density, this corresponds to several kilograms.
Combustion can generate:
CO₂
H₂O
CO
formaldehyde
other oxygenated hydrocarbons
methanol-related fragments
NOₓ from its nitrogen-free combustion environment primarily through atmospheric nitrogen rather than the additive itself
Corrosion inhibitors
A variety of proprietary corrosion-inhibitor packages have been approved for aviation fuels.
Examples appearing in aviation-fuel specifications include products such as:
DCI-4A
DCI-6A
Hitec 580
Nalco 5403
Nalco 5405
Spec-Aid 8Q22
Tolad 351
Tolad 4410
RPS-613
Hitec 515
Mobilad F-800
The exact chemical composition varies by product.
Potential combustion products therefore depend upon the particular formulation but can include:
CO₂
H₂O
CO
aldehydes
hydrocarbons
aromatic compounds
nitrogen-containing products
sulfur-containing products
trace particulate matter
The existence of these additive classes and numerous commercial formulations is documented in aviation-fuel specification summaries.
Biocides
Jet fuel can occasionally be treated with biocides to control microbial contamination.
Examples include:
Biobor JF
Kathon FP 1.5
These are not necessarily continuously present in every tank of aviation fuel.
Biocide-treated fuel can therefore introduce additional:
carbon
hydrogen
oxygen
nitrogen
boron
sulfur
chlorine or other elements
depending upon the particular biocide formulation.
One military/aviation application, for example, specifies Biobor JF with a limit on total boron content.
Lubricating-oil-derived exhaust compounds
Not everything in turbine exhaust originates from the fuel.
Aircraft turbine engines can emit constituents associated with lubricating oils.
Potential constituents include:
hydrocarbons
esters
phosphate-containing compounds
organophosphates
antioxidants
degradation products
metal-containing additives
calcium
magnesium
zinc
phosphorus
sulfur
other trace metals
The aircraft-exhaust literature specifically identifies lubricating-oil combustion/release and mechanical component wear as additional sources of exhaust species beyond the fuel itself.
Engine-wear and corrosion products
Engine components can contribute particulate material through:
bearing wear
seal wear
turbine erosion
compressor erosion
corrosion
thermal degradation
abrasion
Potential elements include:
Iron
Chromium
Nickel
Cobalt
Manganese
Titanium
Aluminum
Silicon
Molybdenum
Tungsten
Copper
Zinc
The exact composition depends strongly upon the alloys and coatings used in the particular engine.
Chlorine-containing compounds
Trace chlorine can enter the combustion system through:
fuel contaminants
additives
environmental contamination
lubrication-system materials
Potential exhaust products include:
HCl
chloride-containing particulate matter
inorganic chlorides
The aircraft particulate literature has detected chlorine among measured elemental constituents.
Phosphorus-containing compounds
Phosphorus can originate particularly from lubricating-oil additives.
Potential products include:
phosphorus oxides
phosphoric acid
phosphate
condensed phosphate compounds
phosphorus-containing particulate matter
Phosphorus has been detected in aircraft exhaust particulate samples.
Silicon-containing compounds
Possible sources include:
lubricating oils
seals
antifoaming additives
engine materials
contamination
Potential exhaust products include:
SiO₂
silicates
silicon-containing particulate matter
Silicon has been measured among aircraft exhaust elemental constituents.
Calcium, magnesium, sodium and potassium compounds
These elements can enter exhaust from:
fuel trace contamination
lubricating oil
additives
engine materials
environmental contamination
Possible exhaust species include:
CaO
MgO
Na₂O
K₂O
carbonates
sulfates
chlorides
phosphates
mixed mineral particles
The exact molecular form depends upon combustion temperature and subsequent plume chemistry.
Iron, chromium, nickel and other transition-metal compounds
Potential compounds include:
Fe
FeO
Fe₂O₃
Fe₃O₄
Ni
nickel oxides
Cr
chromium oxides
Mn
manganese oxides
Cu
copper oxides
Zn
zinc oxide
Some can occur as:
metallic particles
oxide particles
sulfate particles
mixed-metal particles
particles embedded in carbonaceous soot.
Again, detection of an element does not establish that it is present predominantly as a particular chemical compound.
Lead
Lead compounds deserve separate treatment.
Lead is not a normal intentional constituent of modern commercial Jet A/Jet A-1 in the manner that tetraethyl lead is used in aviation gasoline.
Nevertheless, trace lead can potentially occur from:
petroleum contamination
environmental contamination
legacy contamination
materials/wear
The aircraft-exhaust hazardous-air-pollutant literature has historically included lead compounds among measured/recognized aircraft exhaust pollutants.
This should not be interpreted as meaning that modern commercial jet fuel contains large quantities of lead.
Ammonia and secondary nitrogen chemistry
Trace NH₃ may occur in exhaust, while additional ammonia can participate in atmospheric chemistry.
NOₓ oxidation can ultimately generate:
nitric acid — HNO₃
nitrate — NO₃⁻
nitric oxide — NO
nitrogen dioxide — NO₂
nitrate radicals — NO₃
In the atmosphere, these compounds can participate in secondary aerosol formation.
Secondary atmospheric products
The composition immediately at the engine nozzle is different from the composition several seconds, minutes or hours later.
Jet exhaust can undergo atmospheric oxidation, condensation and nucleation.
Potential secondary products include:
Sulfur chemistry
SO₂
SO₃
H₂SO₄
sulfate
bisulfate
ammonium sulfate
Nitrogen chemistry
NO
NO₂
HNO₃
nitrate
NO₃ radicals
peroxyacyl nitrates under suitable conditions
Organic chemistry
Hydrocarbon oxidation can produce:
formaldehyde
acetaldehyde
ketones
organic acids
peroxides
secondary organic aerosol
additional low-volatility organic compounds
Particle chemistry
Particles can acquire:
sulfate
nitrate
ammonium
organic material
water
oxidized hydrocarbons
Consequently, “what comes out of the engine” and “what is eventually found in an aged aircraft plume” are not chemically identical questions.
Condensation-trail-related water and ice
Because hydrocarbon combustion produces large quantities of water vapor, exhaust contains enormous quantities of water immediately after combustion.
For the 1,000-gallon baseline:
~3.7 tonnes of combustion-generated H₂O
Some of that water can condense or freeze under sufficiently cold atmospheric conditions.
The resulting ice particles are therefore principally H₂O, although they may contain or acquire:
sulfate
sulfuric acid
soot
organic material
other trace material
The existence of these ice particles does not imply that the exhaust consists primarily of the trace contaminants; the overwhelming majority of exhaust mass remains ordinary combustion products and entrained atmospheric gases.
Sulfur is already present in the fuel in a great number and variety of chemical compounds. During combustion, the existing sulfur-containing organic molecules are destroyed and their sulfur content is overwhelmingly oxidized to SO₂. Atmospheric oxygen adds oxygen atoms to the fuel sulfur, approximately doubling its mass when expressed as SO₂.
A much smaller and highly variable fraction of that SO₂ is further oxidized to SO₃ and then H₂SO₄, with some of the sulfuric acid subsequently becoming sulfate-containing particulate matter.
Consequently, for a given quantity of fuel, sulfur emissions are approximately proportional to the fuel’s sulfur concentration, while the distribution among SO₂, SO₃, sulfuric acid and particulate sulfate depends strongly on engine operating conditions, plume age, temperature, humidity and atmospheric chemistry.
Sulfur-containing compounds
Jet fuel contains organically bound sulfur unless it has been highly hydrotreated or otherwise desulfurized.
Sulfur chemistry is particularly important because sulfur in fuel does not simply disappear during combustion.
Sulfur dioxide — SO₂
The principal direct sulfur combustion product.
Approximate calculation:
For sulfur concentration 600 ppm by mass:
3,028 kg fuel × 0.000600 = 1.817 kg sulfur
If converted completely to SO₂:
1.817 × (64.066/32.065) ≈ 3.63 kg SO₂
Thus, at 600 ppm sulfur:
~3.6 kg SO₂ per 1,000 gallons
For comparison, at the ASTM Jet A maximum sulfur concentration of approximately 3,000 ppm:
3,028 × 0.003 = 9.08 kg sulfur
Complete conversion to SO₂ gives:
~18.2 kg SO₂ per 1,000 gallons
Actual SO₂ emissions depend upon the fuel sulfur content and sulfur-conversion chemistry.
Sulfur trioxide — SO₃
A smaller fraction of sulfur is oxidized beyond SO₂ to SO₃.
Sulfuric acid — H₂SO₄
SO₃ reacts rapidly with water:
SO₃ + H₂O → H₂SO₄
Sulfuric acid may subsequently condense or participate in formation/growth of ultrafine particles.
Sulfate
Exhaust sulfur can therefore ultimately appear as:
sulfuric acid
bisulfate
sulfate
ammonium sulfate
other sulfate-containing aerosol species
Sulfur is commonly the dominant measured elemental component of aircraft exhaust particulate matter. One aircraft-exhaust study found total measured elemental emissions of approximately 6.3–27.5 mg/kg fuel, with sulfur accounting for approximately 54–80% of that elemental mass.
For 3,028 kg fuel, that elemental-emission range corresponds to approximately:
19–83 grams of measured elements per 1,000 gallons
This is elemental material measured in particulate samples—not total sulfur emissions.
A consolidated chemical inventory
A practical “master list” of chemical substances and species potentially associated with petroleum-jet-engine exhaust therefore includes:
Major gases
N₂
O₂
CO₂
H₂O
CO
Nitrogen oxides
NO
NO₂
N₂O
HNO₃
NO₃
nitrate
trace NH₃
other nitrogen-containing species
Sulfur compounds
SO₂
SO₃
H₂SO₄
sulfate
bisulfate
ammonium sulfate
sulfur-containing organic compounds
sulfur-containing particulate matter
Unburned hydrocarbons
methane
ethane
propane
butanes
pentanes
hexanes
heptanes
octanes
higher alkanes
alkenes
alkynes
cycloalkanes
aromatic hydrocarbons
Aromatics
benzene
toluene
ethylbenzene
xylenes
trimethylbenzenes
styrene
naphthalene
alkyl naphthalenes
Oxygenated organics
formaldehyde
acetaldehyde
propionaldehyde
acrolein
benzaldehyde
acetone
methyl ethyl ketone
formic acid
acetic acid
propionic acid
phenol
cresols
Polycyclic Aromatic Hydrocarbons
naphthalene
acenaphthylene
acenaphthene
fluorene
phenanthrene
anthracene
fluoranthene
pyrene
benz[a]anthracene
chrysene
benzo[b]fluoranthene
benzo[k]fluoranthene
benzo[a]pyrene
indeno[1,2,3-cd]pyrene
dibenz[a,h]anthracene
benzo[ghi]perylene
Carbonaceous particulate matter
elemental carbon
soot
black carbon
organic carbon
condensed hydrocarbons
PAH-containing particles
Inorganic elements detected in aircraft particulate matter
Magnesium
Silicon
Phosphorus
Sulfur
Clorine
Potassium
Calcium
Titanium
Chromium
Manganese
iron
Nickel
Copper
Zinz
Bromine
Silver
Indium
Antimony
Tellurium
Iodine
Thallium
Aircraft particulate measurements have specifically reported this broad elemental suite.
Additional potentially relevant trace metals
Depending upon fuel, lubricant, contamination and engine materials:
Vanadium
Cobalt
Aluminum
Molybdenum
Tungsten
Lead
Arsenic
Cadmium
Mercury
Selenium
Tin
The presence and concentration of these elements are highly variable and should not be treated as universal constituents of every jet exhaust plume.
CLARIFICATION #1:
Some astute readers have pointed out that aircraft pollutants are relatively small compared to planetary forces. That is mostly (but not completely) true, but nevertheless, such a comparison is NOT the most appropriate perspective.
The massive numbers associated with pollution caused by aviation and rocketry are presented so that they can be compared to the purported and unproven amounts of aluminum, barium, strontium, coal fly ash or whatever other substances many people claim are being sprayed into the atmosphere to create the white lines in the sky.
Any purported “spraying” should be viewed in comparison to the massive amount of pollutants that are being spewed into the atmosphere every day by the aviation and rocketry industries.
CLARIFICATION #2:
Nothing in this information is designed to support “de-growth” or “sustainability” as it is promoted by the United Nations Agenda 2030 or any other groups. The information contained in this article supports removing compounds from jet fuel and aviation gasoline that can easily be removed in order to reduce pollution.
On page 29 (page 31 in the PDF) in the 2025 Statistical Review of World Energy, you can verify that in 2024, 119,558,670,000 gallons of jet fuel were used worldwide.
7,799,000 barrels x 42 gallons/barrel x 365 days = 119,558,670,000 gallons
119,558,670,000 gallons of jet fuel x 6.7 pounds per gallon = 800+ billion pounds
In the subtitle of this article, I posed the following question:
The United States, other governments, and private actors are engaging in the manipulation of the Earth’s weather by, inter alia:
a. allowing chemical/condensation trails to accumulate behind airplanes on a massive scale, dramatically altering the Earth’s atmosphere, temperature and weather;
b. allowing the chemical composition of jet fuel to be of such a quality that it alters the trails left behind airplanes, dramatically altering the Earth’s atmosphere, temperature and weather;
c. allowing particulate matter and other contaminants to create trails behind airplanes, dramatically altering the Earth’s atmosphere, temperature and weather;
https://thegeofight.com/documents/mabie-v-university-of-colorado-amended-complaint.pdf
What if all of “us” are the “unwitting geoengineers?”
Contrails are a concern in climate studies as increased jet traffic may result in an increase in cloud cover. Several scientific studies are being conducted with respect to contrail formation and their climatic effects. Cirrus clouds affect Earth’s climate by reflecting incoming sunlight and inhibiting heat loss from the surface of the planet.
It has been estimated that in certain heavy air-traffic corridors, cloud cover has increased by as much as 20%.
Since contrails can spread out and essentially become cirrus clouds, it is felt that contrails may affect the planetary climate in similar ways. Other studies are underway to better understand the role that jet exhaust itself plays in modifying the chemistry of the upper levels of the atmosphere.
Watch the video below:
Artificial Intelligence Analysis
Based on a suggestion from a good friend (you know who you are!) I decided to use the advanced tools of the “powers that be” against the “powers that be.”
I “tricked” ChatGPT and Google Gemini into thinking that I was proposing an actual geoengineering/weather modification project and ChatGPT and Google Gemini dutifully provided the “scientific” analysis presented in this article, because those programs did not recognize the true context of my request. Google Gemini provided the first two sections of this article (Particulate Matter and Water) as well as much of the specific data, and ChatGPT provided the remainder of the article and most of the graphics as well.
This article is NOT about what “THEY” are “spraying.”
This article actually describes the current state of the world in which we live. Some people refer to it as “accidental geoengineering.” The details are as accurate as possible. This is the sum total of the harm that the global aviation and rocket industries have been doing to planet Earth. Maybe we are also being “sprayed” by some hidden evil villains - but our planet is clearly being poisoned by corporate interests and by the regular people who unwittingly support them.
Reality
The information in this article is about what “we” (humanity) are collectively doing to ourselves through the massive pollution that is directly and demonstrably caused by global aviation and rocketry.
“We the People” have been implementing “Project InHumanity” on ourselves for over one hundred years (since the beginning of aviation and rocketry). Did you comprehend the double entendre in the title? It may be even deeper than you think!
The chemicals listed in this article are chemicals that are found in the exhaust of aircraft that use jet fuels, light aircraft that use leaded AvGas, and rockets that use a wide variety of fuels.
Jet Engine Exhaust Pollution Trails
What happens when super-heated boiling water in a pressurized pot (jet engine) is heated to 900-1500°F, mixed with several hundred quintillion onion-shaped graphene-like carbon based micro-particles nucleated by the various elements found in jet fuel, jet fuel additives and worn engine parts such as aluminum, barium, calcium, chromium, copper, iron, lead, magnesium, manganese, nickel, niobium, potassium, scandium, selenium, strontium, sulphur, tin, titanium, vanadium and zirconium, and then the contents of the pot are deposited into an ice-supersaturated region in the upper troposphere?
COMMERCIAL AVIATION (Jet Fuel)
Globally, on an average day, there are over 100,000 commercial flights.
https://www.oag.com/airline-frequency-and-capacity-statistics
Approximately 100 billion gallons of jet fuel are consumed each year. Approximately 5% of the miles flown are through ice supersaturated regions.
Every day, everywhere, every plane, every helicopter and every jet (commercial, private and military) is spewing a trail of chemicals across your clear blue sky, but by law, it is invisible.
It must be acknowledged that the exhaust from jet fuel is being deposited in the atmosphere whether or not any covert geoengineering and/or weather modification programs are occurring.
LIGHT AIRCRAFT (Leaded AvGas)
Approximately 200 million gallons of leaded Aviation Gas are combusted and deposited into the atmosphere globally every year.
CLICK HERE to read an important article about leaded Aviation Gas
ROCKETS (Aluminum and/or Kerosene)
The rocket industry is enormous
https://ensun.io/search/rocket-manufacturing
Aluminum Rocket Fuel
As evidenced below, it is extremely difficult to pinpoint accurate estimates of the amount of aluminum that international rocketry (public, private and military) have emitted into the atmosphere.
The vast majority of people are unaware that solid rocket fuel often utilizes aluminum as a propellant.
Several currently active, high-power rockets and boosters utilize powdered aluminum (typically 14-20% by weight) in their solid rocket propellant to enhance performance and boost combustion temperature. Key examples include NASA’s Space Launch System (SLS) boosters, Ariane 6, Vega, and Atlas V (via GEM-63 boosters).
Space Launch System (SLS): Uses two solid rocket boosters that burn a mixture of ammonium perchlorate, aluminum powder, and a binder.
Ariane 6 & Vega: The European Space Agency’s rockets rely on solid boosters using aluminum powder for fuel.
Atlas V & Vulcan Centaur: Utilize Northrop Grumman’s GEM 63 and GEM 63XL solid boosters, respectively.
Military & Launch Vehicles: Many tactical missiles and smaller launch vehicles (e.g., Pegasus) use aluminum-based solid propellants.
How much aluminum is in the two solid fuel boosters in NASA’s Artemis Space Launch System?
Each of Artemis’s two solid rocket boosters containing roughly 1.1 million pounds to 1.5 million pounds of propellant. The propellant is a mixture of Ammonium Perchlorate (oxidizer), aluminum (fuel), iron oxide (catalyst), and a PBAN copolymer binder. The propellant contains approximately 16% aluminum powder by weight within its solid propellant mixture.
This equates to roughly 176,000 to 240,000 pounds of aluminum powder per booster for a total of 352,000 and 480,000 pounds of aluminum.
The aluminum that will be spewed into the atmosphere by just one launch of the Space Launch System is comparable to the combined weight of every football player in the NFL!
The Space Launch System also utilizes polybutadiene acrylonitrile (PBAN) copolymer, a compound used most frequently as a rocket propellant fuel mixed with ammonium perchlorate oxidizer. It was the binder formulation widely used on the 1960s–1970s big boosters (e.g., Titan III and Space Shuttle SRBs). It is also notably used in NASA’s Space Launch System, likely reusing the design from its Space Shuttle counterpart. PBAN is normally cured with the addition of an epoxy resin.
The Solid Rocket Boosters for the Space Launch System emit a combination of
Aluminum oxide Al2O3
Hydrogen chloride HCl
Water vapor H2O
Carbon dioxide CO2
Nitrogen oxides NOx
The propellant mixture consists primarily of ammonium perchlorate (oxidizer), aluminum powder (fuel), and a PBAN (polybutadiene acrylonitrile) binder. While the primary emission is Al2O3, the solid-fueled rocket boosters release significant amounts of acidic chlorine-based gases and greenhouse gases into the upper atmosphere.
The two solid rocket boosters used by the Space Shuttle utilized propellants based on aluminum.
ARTEMIS SOLID FUEL ROCKETS
Ariane (European Space Agency)
SOUNDING ROCKETS
The term originates from “sondare” or “sond,” referencing the act of surveying or probing for data. Sounding rockets are named after the nautical term “to sound,” which means to measure or take soundings (such as measuring water depth with a weighted line). These suborbital rockets are designed to carry scientific instruments into the upper atmosphere to measure, probe, and sample the environment.
They measure atmospheric properties, test satellite instruments, and study the sun or space, providing data from areas too high for balloons and too low for satellites. They follow a parabolic trajectory (going up and coming down) rather than entering orbit, typically lasting about 15 minutes. Since 1958, NASA has used them for quick, low-cost scientific, and solar research.
https://www.nasa.gov/soundingrockets/
Sounding rockets can be single or multi-stage vehicles, such as the Orion or Black Brant.
Sounding rockets are suborbital vehicles designed to carry scientific instruments into the upper atmosphere altitude for short-duration studies. They do not reach orbital velocity, following a parabolic trajectory that allows them to collect data for 5–20 minutes before returning to Earth. These rockets provide a cost-effective, quick-turnaround method to study auroras, solar physics, and the atmosphere in regions too low for satellites.
Key Launch Sites: Major activity occurs at Wallops Flight Facility (VA), White Sands Missile Range (NM), Poker Flat (AK), and Andøya Rocket Range (Norway).
Sounding rockets are primarily used for atmospheric, ionospheric, and solar research, as well as astronomy. Sounding rockets are often used for testing instruments before they are deployed on satellites and are essential for researching the Earth’s environment. They are the only platforms that can perform in-situ measurements in the mesosphere and lower thermosphere so they are often launched from various locations worldwide to target specific scientific events.
Auroral Zone Upwelling Rocket Experiment (AZURE)
NASA successfully launched the Auroral Zone Upwelling Rocket Experiment or AZURE mission on April 5 from the Andøya Space Center in Norway.
Two Black Brant XI-A sounding rockets were launched at 6:14 and 6:16 p.m. EDT on April 5 carrying scientific instruments for studying the energy exchange within an aurora.
The AZURE mission is designed to make measurements of the atmospheric density and temperature with instruments on the rockets and deploying visible gas tracers, trimethyl aluminum (TMA) and a barium/strontium mixture, which ionizes when exposed to sunlight. The vapors were released over the Norwegian Sea at 71 through 150 miles altitude.
These mixtures, using substances similar to those found in fireworks, created colorful clouds that allow researchers to track the flow of neutral and charged particles with the auroral wind. By tracking the movement of these colorful clouds via ground-based photography and triangulating their moment-by-moment position in three dimensions, AZURE will provide valuable data on the vertical and horizontal flow of particles in two key regions of the ionosphere over a range of different altitudes.
https://www.nasa.gov/solar-system/nasa-launches-two-rockets-studying-auroras/
Colorful clouds formed by the release of vapors from the two AZURE rockets allow scientist to measure auroral winds.
Credits: NASA/Lee Wingfield
SPACEX FALCON 9
SPACEX FALCON HEAVY
GLOBAL MILITARY
PATRIOT MISSILES
UKRAINE AND RUSSIA
HYPERSONIC MISSILES
IRAN
NORTH KOREA
Space Pollution
This study presents the first measurement of upper-atmospheric pollution resulting from space debris re-entry and the first observational evidence that the ablation of space debris can be detected by ground-based lidar.
Our findings demonstrate that identifying pollutants and tracing them to their sources is achievable, with significant implications for monitoring and mitigating space emissions in the atmosphere.
1. Micro-particulate Matter:
350 septillion individual pieces of Particulate Matter (PM2.5) which included 27.2 million pounds of onion-shaped, carbon-based, graphene-like particles.
Approximately 350 SEPTILLION pieces of PM2.5 particulate matter are released into the earth’s atmosphere every year.
Aircraft emissions of ultrafine particles characterized by real-world near runway measurements
https://pmc.ncbi.nlm.nih.gov/articles/PMC12176625/
The Weight-Count Paradox: Aircraft emit a disproportionately high number of ultrafine particles (sub-0.1 $\mu m$).
Releasing 350 septillion PM2.5 microparticles into the upper atmosphere (30,000–40,000 feet) every year constitutes an unprecedented, catastrophic alteration of the Earth’s atmosphere, leading to severe, long-term environmental and public health crises.
Note: 350 septillion is an astronomically high number of particles. For context, it is roughly comparable to the number of stars in the observable universe and the estimated total number of bacteria on Earth, highlighting that this is a scenario of massive, almost unimaginable scale.
Based on general principles of atmospheric science and 𝑃𝑀2.5 health impacts, here are the expected consequences:
Black Carbon
Climate & Weather Effects
• Strong absorber of sunlight — contributes to atmospheric warming. Black carbon deposited on snow/ice accelerates melting (albedo reduction).
• Alters temperature gradients, with potential to weaken monsoon systems in some areas, intensify droughts, or shift rainfall belts.
• Particles that are deposited into the lower regions of the stratosphere can self-loft into higher regions of the stratosphere where they can remain far longer than particles deposited in the lower troposphere.
Human Health
• A major component of particulate matter (PM₂.₅), linked to respiratory and cardiovascular disease, cancer risk, and impacts on birth outcomes.
• High concentrations can cause lung inflammation, reduced lung function, and increased mortality.
A. Blocking Sunlight and Climate Cooling
Massive Reduction in Sunlight: Such an enormous volume of particles would act as a highly effective, persistent shield against incoming solar radiation, causing significant “global dimming.”
Artificial Cooling: These particles would scatter sunlight back into space, leading to a rapid, drastic drop in global temperatures, potentially triggering a synthetic, long-term winter-like state.
Altered Precipitation Patterns: The particles would likely act as cloud condensation nuclei (CCN), altering cloud properties, reducing rainfall in many areas, and disrupting global water cycles.
B. Catastrophic Health Impacts
Long-Range Transport: Even though released at high altitudes, these fine particles would eventually settle into the troposphere, spreading globally via jet streams and settling over inhabited areas.
High-Altitude Pollution: 𝑃𝑀2.5 is a major cause of premature death (7–9 million annually currently). A massive influx would exponentially increase rates of cardiovascular disease, lung cancer, stroke, asthma, and dementia.
Systemic Toxicity: 𝑃𝑀2.5 particles can pass directly into the bloodstream and alveoli, causing chronic inflammation, oxidative stress, and reducing life expectancy globally.
C. Atmospheric and Environmental Destruction
Stratospheric Chemistry Changes: Releasing these particles at 30,000–40,000 feet (the upper troposphere/lower stratosphere) could introduce them directly into the ozone region. The particles could provide surfaces for chemical reactions that destroy the ozone layer.
Acidification and Ecosystem Damage: As these particles settle, they would cause severe acidification of lakes, streams, and soil, damaging ecosystems and destroying biodiversity.
Reduced Visibility: The sky would likely appear hazy or grayish globally, with significantly reduced visibility and constant, thick, long-lasting haze (a phenomenon similar to, but far worse than, extreme wildfire smoke).
D. Continuous, Cumulative Damage
No “Clearing” Effect: Because the emissions are yearly and constant, the particles would accumulate faster than they can be removed by natural precipitation and gravitational settling, leading to a relentless worsening of environmental conditions.
Visibility and Climate: The cumulative nature of the release means that the reduction in sunlight and air quality would grow more severe each year.
Air pollution from aircraft jet engines is a significant environmental and public health problem.
A single jet engine can release approximately one quadrillion to one hundred quadrillion particles per kilogram of fuel burned. Given that large commercial jet engines can consume significant amounts of fuel per second, this translates to a massive rate of emission. At the engine exit, concentrations can reach approximately one billion particles per cubic centimeter.
Microparticles from jet engine exhaust (specifically ultrafine particles <100 nanometers) cause significant health issues by penetrating deep into the lungs and entering the bloodstream, potentially spreading to the heart and brain. The complex, sub-microscopic, and often toxic nature of these emissions, particularly in high-traffic, low-altitude areas near airports, presents a significant, yet largely overlooked, public health risk.
Exposure to these microparticles is linked to respiratory issues such as asthma, cardiovascular diseases, cancer, impaired neurological function and even Autism Spectrum Disorder.
NOTE FOR THE GRAPHIC BELOW: 10 to the 15th power is 1 quadrillion, 10 to the 16th is 10 quadrillion and 10 to the 17th power is 100 quadrillion particles per second.
SOURCE:
https://www.nature.com/articles/s41612-023-00477-1#Fig5
Google’s AI Overview referenced the same study that I used, stating that jet engines emit approximately 347 SEPTILLION individual particles per year.
Google’s AI Overview estimated that jet engines emit between one million and one billion ultra-fine particles per cubic centimeter.
2. Water Vapor:
125 billion gallons (1 trillion pounds) of water.
This is approximately half the volume of water in Upper Klamath Lake in Oregon.
Releasing 125 billion gallons of water vapor (over one trillion pounds) annually at 30,000–40,000 feet—altitudes corresponding to the upper troposphere/lower stratosphere—would function as a consistent, localized injection of a potent greenhouse gas, leading to increased regional and global warming, enhanced cloud formation, and accelerated climate feedback loops.
Contrails and induced cirrus are widely regarded as a significant climate forcing mechanism, potentially comparable to or greater than CO₂ alone in warming impact.
Based on atmospheric science and aviation emission studies, the impacts include:
A. Enhanced Greenhouse Effect and Atmospheric Warming
Water Vapor as a Greenhouse Gas: Water vapor is the most abundant natural greenhouse gas. While its lifetime in the troposphere is short, it absorbs heat radiated from Earth, preventing it from escaping to space.
Amplification of Warming: Increased water vapor in the upper atmosphere amplifies the warming effect of other greenhouse gases, acting as a positive feedback loop.
Upper Atmosphere Sensitivity: Water vapor at high altitudes is particularly effective at trapping heat, where even small increases can have a disproportionate impact on climate.
B. Increased Cloud Formation
Increased Cloud Cover: At 30,000–40,000 feet, ambient temperatures are very low. The released water vapor, combined with soot particulates from engines, would create persistent and potentially growing cloud cover if it were released in Ice super-saturated regions. These regions make up approximately 5% of the airspace. The reflective nature of white clouds would have a cooling effect.
Invisible Water Vapor: Approximately 95% of the troposphere and tropopause and 100% of the stratosphere are not conducive to the creation of ice clouds (humidity is too low). Therefore the deposition of large amounts of water vapor would have a significant warming effect.
C. Disruption of Regional Weather Patterns
Water Cycle Intensification: Increased water vapor amplifies the global water cycle, making wet regions wetter and dry regions drier.
Intense Storms: The added vapor increases the latent energy in the atmosphere, which can fuel more intense storms and increase extreme weather events, particularly over land.
D. Climate Feedbacks and Long-Term Impact
Positive Feedback Loop: Higher temperatures caused by this water vapor increase the atmosphere’s ability to hold moisture, leading to more water vapor, accelerating the warming.
Stratospheric Impact: If this vapor reaches the stratosphere, it can remain longer than in the troposphere, leading to significant, long-lasting warming.
Context: While 125 billion gallons seems massive, it is relatively small compared to natural atmospheric water cycles (e.g., millions of tons of water vapor are added daily through natural evaporation). However, the concentration of this injection at high altitudes (where the air is usually very dry) makes it a significant, artificial contributor to climate change.
In short, such a project would create a planet-wide, self-induced environmental disaster, causing catastrophic damage to human health, biodiversity, and the global climate.
3. Carbon Dioxide (CO₂)
2.15 trillion pounds of carbon dioxide
Climate & Weather Effects
• Primary greenhouse gas — cumulative increases trap infrared radiation, warming the planet.
• Warming alters jet streams, storm tracks, precipitation patterns, and can intensify extreme weather (heatwaves, droughts, heavy rainfall events).
• Ocean acidification from CO₂ uptake alters marine ecosystems.
Human Health
• At ambient levels, CO₂ itself is not highly toxic, but climate change driven by high CO₂ harms health through heat stress, vector-borne disease shifts, food/water insecurity, and air quality degradation.
4. Carbon Monoxide (CO) ☠️
1.14 billion pounds of carbon monoxide
Climate & Weather Effects
• Indirect greenhouse influence by altering atmospheric chemistry (affects methane lifetime).
• Not a major direct driver of climate compared to CO₂ or methane.
Human Health
• Very toxic; binds to hemoglobin more strongly than oxygen, reducing oxygen delivery.
• Symptoms include headache, dizziness, confusion, unconsciousness, and death at high exposure.
• Large atmospheric concentrations could cause widespread poisoning indoors and outdoors
Google’s AI Overview provided a similar result:
.
5. Sulfur Oxides (SO₂ / SO₃)
350 to 700 million pounds of sulphur dioxide
Climate & Weather Effects
• SO₂ oxidizes to sulfuric acid particles — these scatter sunlight and increase Earth’s albedo, potentially causing temporary cooling (stratospheric aerosols did this after volcanic eruptions).
• Can alter precipitation patterns and regional circulation if widespread.
Human Health
• SO₂ is irritating and can trigger asthma and broncho-constriction.
• Sulfuric acid aerosols damage lungs and can lower life expectancy.
• Acid rain from sulfur oxides harms vegetation, soils, and aquatic ecosystems.
Google’s AI Overview provided a substantially larger estimate:
(This is a good example of why you should NOT trust Artificial Intelligence. In short, the answer received from Google AI is an absolute mess. Firstly, it confused the terms sulfur and sulfur dioxide. Secondly, the summary at the top of the response claims that 3.5-4.2 billion pounds of sulfur dioxide are released, but the summary at the bottom of the response claims a more accurate amount of 700 million pounds. I used the lower amounts and double checked from other sources. )
6. Nitrogen Oxides (NOₓ: NO + NO₂)
100 to 120 million pounds of nitrogen oxides
Climate & Weather Effects
• Precursors to ozone (a greenhouse gas at ground level) and nitrate aerosols, which scatter sunlight.
• NOₓ emissions can cool the climate slightly via aerosol formation but increase ozone warming and contribute to smog.
• Can change nitrogen deposition rates, affecting ecosystems and cloud chemistry.
Human Health
• NO₂ irritates respiratory system — increases asthma, bronchitis, and other pulmonary problems.
• Contributes to secondary particulate matter formation (nitrates), further harming health.
7. Naphthalene
CLICK HERE FOR ADDITIONAL DETAILS
8. Aluminum (From rocket exhaust)
11 million pounds of aluminum powder
Climate & Weather Effects
• Can scatter and absorb sunlight, altering Earth’s radiative balance. At very high concentrations this could cool the surface locally (a bit like stratospheric aerosols), but interactions are unpredictable and could disrupt regional weather patterns (e.g., monsoons).
• Smaller particles can serve as cloud condensation nuclei, changing cloud properties, rainfall distribution, and potentially weakening some storm systems while intensifying others.
Human & Ecosystem Health
• Inhalation risk: ultrafine aluminum particles are respirable and can penetrate deep into lungs, potentially causing inflammation or neurotoxicity.
• Chronic exposure may exacerbate asthma, cardiovascular issues, and neurological disorders (some studies link aluminum to cognitive effects, though mechanisms aren’t fully settled).
• Ecotoxicity: settles on soils and water bodies, can harm microbial activity and aquatic life.
9. Magnetite
8-10 million pounds of magnetite
Magnetite is a black, opaque, and highly magnetic iron oxide mineral (Fe3O4) that acts as one of the primary, highest-quality ores of iron. As the most strongly magnetic naturally occurring mineral, it is found in igneous, metamorphic, and sedimentary rocks, often appearing as “black sand” on beaches.
Magnetite (Fe3O4) in jet engine emissions is an increasingly studied particulate pollutant. Primarily generated by the extreme temperatures of aviation combustion and the wear of engine components, these ultrafine magnetic nanoparticles pose growing health concerns due to their ability to easily enter the bloodstream and bypass the blood-brain barrier. [1, 2, 3, 4]
Origins of Magnetite in Jet Exhaust
Combustion of Traces: Modern jet fuel is highly refined, but jet turbine lubricants and trace metals in the fuel can undergo high-temperature combustion, producing iron-oxide nanoparticle aggregates. [1, 2, 3]
Engine Wear: Jet engines rely on advanced superalloys (such as Inconel, which contains iron, nickel, and chromium) for their high-stress, high-temperature components. Thermal stress, friction, and oxidation of these parts release metal-rich ultrafine particles (UFPs) into the exhaust stream. [1, 2]
Size and Behavior
Nanoscale Properties: Unlike the millimeter-sized magnetite particles found in industrial fly ash, the magnetite found in jet and diesel exhaust is largely dominated by ultrafine particles (<0.1μm in diameter). [1, 2, 3]
Dispersion: Because they are extremely light and small, these particles are easily suspended in the air. High-altitude emissions disperse widely, while ground-level emissions contribute significantly to poor air quality around airports, particularly during taxiing and take-off. [1]
Health & Environmental Implications
Neurological Risks: Ultrafine magnetite can bypass the lungs and directly enter the bloodstream or travel up the olfactory bulb, making its way into the brain. Research has linked these anthropogenic magnetite nanoparticles to neurodegenerative diseases (like Alzheimer’s and Parkinson’s). [1, 2, 3, 4, 5]
Cardiovascular Disease: Exposure to these particles is known to induce oxidative stress and chronic inflammation in cardiovascular and respiratory systems. [1, 2, 3]
Electromagnetic Resonance: Because magnetite is highly magnetic, scientists have discovered that these particles have strong electromagnetic absorption properties (which is actively studied in the context of cell phone radiation and cellular damage). [1]
Jet engines and their associated combustion processes emit significantly more magnetite (Fe3O4) than hematite (Fe2O3). [1]
The iron oxide emissions from jet exhaust primarily consist of trace metals from engine wear and fuel impurities, which form nanocrystals in the high-temperature, reducing environment of the engine core. Here is a closer look at the emissions: [1]
Magnetite dominance: Because the primary combustion chamber of a jet engine operates in a highly fuel-rich and low-oxygen state (a “reducing” environment), the iron particulates that form largely oxidize into magnetite. [1, 2, 3]
Minor hematite: Hematite requires highly oxidizing conditions, making it a relatively minor component of engine exhaust, though it can still be found in smaller quantities. [1, 2]
Brake vs. Exhaust differences: While jet engines emit more magnetite in their exhaust, it is worth noting that aircraft brakes (and automotive brake debris in general) primarily emit hematite. [1]
10. Lead (From Light Aircraft Exhaust)
10 to 20 million pounds
Lead is a toxic heavy metal with no known safe level of exposure. As fine particulate matter (approximately 13 nanometers in size), lead is small enough to easily penetrate mucosal barriers and enter the bloodstream.
Impact on Children: Children are the most vulnerable due to their developing nervous systems. Exposure is linked to:
Irreversible cognitive damage, including reduced IQ, decreased academic performance, and learning difficulties.
Behavioral issues, such as decreased ability to pay attention and increased behavioral problems.
Permanent physiological changes, including the inhibition of calcium pathways in neurons.
Impact on Adults: Long-term exposure in adults is associated with:
Cardiovascular issues, including high blood pressure, hypertension, and an increased risk of death from cardiovascular disease.
Organ damage, specifically affecting the kidneys and immune system.
Reproductive problems in both men and women.
Neurological concerns, with some evidence suggesting a possible link to dementia.
11. Semi-Volatile Polycyclic Aromatic Hydrocarbons
480,000 to 910,000 pounds
• Exposure to hydrocarbons and associated particulate matter (specifically ultrafine particles, UFP <100 nm) can cause coughing, labored breathing, and worsen asthma or chronic respiratory conditions.
• Some polycyclic aromatic hydrocarbons are classified as known or probable carcinogens. They are associated with increased risks of lung and bladder cancer, particularly among airport ground personnel.
• Chronic exposure has been linked to neurological damage, including headaches, dizziness, fatigue, cognitive impairment, and in some cases, peripheral neuropathy.
• Acute Toxicity: High-level exposure to can cause immediate symptoms like nausea, vomiting, and in extreme cases, unconsciousness.
☠️ Hydrazines (e.g., N₂H₄)
Climate & Weather Effects
• Do not persist in the atmosphere long but break down to nitrogen, ammonia, and other nitrogen species that can contribute to smog and nitrogen deposition.
Human Health
• Extremely toxic by inhalation and dermal exposure. Causes irritation of eyes/respiratory tract, neurological effects, liver/kidney damage, and is a potential carcinogen.
• Even moderate ambient levels would pose serious public health risk.
Hydrogen Chloride (HCl)
Climate & Weather Effects
• Highly soluble in water — rapidly forms hydrochloric acid in clouds/rain. This would cause acid rain, damaging forests, soils, and water bodies.
Human Health
• Corrosive gas — irritates eyes, skin, and lungs. At high concentration, can cause pulmonary edema and death.
• Background increases would worsen respiratory diseases like asthma.
Hydroxyl Radicals (OH)
Hydroxyl radicals are a short-lived atmospheric reactive species.
Climate & Weather Effects
• The primary danger caused by hydroxyl radicals is the rapid, sunlight-driven conversion of other compounds into a high volume of hazardous secondary organic aerosols (fine particulate matter). These highly reactive hydroxyl radicals act as oxidants, reacting with hydrocarbons to produce 35 times more particles than initially emitted, significantly increasing the concentration of toxic soot and aerosols.
• Perturbations could disrupt atmospheric oxidation capacity, altering lifetimes of many gases.
Human Health
• Hydroxyl radicals drive the chemistry that converts emitted vapors into solid, breathable particles (submicrometer particles). They react almost instantly and the resulting particulate matter is small enough to lodge deep in the human lungs and enter the bloodstream, contributing to cardiovascular issues, cancer, and respiratory disease.
12. Trace Minerals
Information coming soon.
🧠 Summary Table
🌦 Broad Takeaways
✅ Climate
• Black carbon is one of the most significant climate drivers based upon its ability to absorb and re-radiate heat
• Sulfur oxides can temporarily cool but at great environmental cost.
☁️ Weather Patterns
• Aerosols and reactive gases can alter cloud formation and rainfall unpredictably. Large perturbations can disrupt monsoons, storm tracks, and drought/flood balances.
🫁 Human Health
• Many of these substances are either toxic directly (e.g., CO, hydrazines, HCl) or contribute to secondary pollutants (ozone, particulate matter) that harm respiratory and cardiovascular health.
I. SYSTEM-LEVEL OVERVIEW
Large-scale atmospheric geoengineering involving aluminum, black carbon, sulfur oxides, nitrogen oxides, and reactive gases would not act as a single intervention. Instead, it would create a multi-layered chemical forcing event affecting:
• Earth’s radiative balance
• Atmospheric chemistry and oxidation capacity
• Cloud microphysics and precipitation
• Global circulation systems
• Human respiratory, cardiovascular, neurological, and immune health
• Terrestrial and aquatic ecosystems
These systems are non-linear, meaning small changes can trigger outsized or irreversible effects.
II. RADIATIVE FORCING & ENERGY IMBALANCE
Key Mechanisms
A. Solar Reflection vs Absorption
Sulfur oxides and some aluminum aerosols scatter sunlight → surface cooling
Black carbon absorbs sunlight → atmospheric heating
Mixed aerosol fields can destabilize temperature gradients
B. Vertical Heating Asymmetry
Heating aloft + cooling below can:
• Suppress convection
• Trap pollutants near the surface
• Alter jet stream behavior
Potential Outcomes
• Regional cooling with global instability
• Increased heat waves in some regions
• Accelerated polar ice melt (black carbon deposition)
• Disruption of seasonal climate cycles
III. DISRUPTION OF WEATHER PATTERNS
🌧 PRECIPITATION & CLOUD DYNAMICS
Aerosol Overloading Effects
• Increased cloud condensation nuclei → smaller droplets
• Delayed rainfall → longer droughts
• Sudden precipitation release → flooding events
Observed Risks (from volcanic & pollution analogs):
Weakening of monsoon systems
Poleward shift of rainfall belts
Reduced soil moisture persistence
More intense but less frequent storms
🌪 ATMOSPHERIC CIRCULATION CHANGES
• Altered Hadley Cell strength
• Jet stream destabilization
• Increased atmospheric blocking events
• Persistent heat domes or cold stagnation zones
Net Result:
⚠️ Weather becomes less predictable and more extreme, not more controlled.
IV. ATMOSPHERIC CHEMISTRY CASCADE EFFECTS
A. Hydroxyl Radical (OH) Disruption
Large chemical injections may:
• Reduce methane breakdown
• Extend lifetimes of toxic gases
B. Ozone & Secondary Pollutants
Consequences
• Reduced ozone allows additional ultraviolet radiation to reach the earth’s surface
• Ultraviolet C that is normally blocked may pass through reduced ozone layers
C. Acid Deposition
Sulfur oxides + nitrogen oxides → acid rain
Impacts
• Soil nutrient leaching
• Forest canopy damage
• Fish and amphibian population collapse
• Corrosion of infrastructure
V. HUMAN HEALTH IMPACTS
🫁 RESPIRATORY SYSTEM
Particulate Matter (PM₂.₅ & Ultrafines)
• Deep lung penetration
• Chronic inflammation
• Reduced lung capacity
• Asthma exacerbation
• Increased pneumonia risk
❤️ CARDIOVASCULAR EFFECTS
Particles enter bloodstream →
• Endothelial dysfunction
• Increased clot formation
• Elevated heart attack and stroke risk
🧠 NEUROLOGICAL & SYSTEMIC EFFECTS
Nanoparticles (e.g., aluminum):
• Can cross blood–brain barrier
• Neuroinflammatory responses
• Cognitive and motor impacts (under investigation)
☠️ ACUTE TOXICITY RISKS
Hydrazines & Hydrogen Chloride
• Highly corrosive and toxic
• Eye, skin, and lung injury
• Potential carcinogenicity
• Emergency-level exposure risk even at low concentrations
Carbon Monoxide
• Oxygen displacement
• Headaches, confusion, loss of consciousness
• Fatal at elevated levels
VI. ECOLOGICAL & BIOSPHERE DAMAGE
🌱 TERRESTRIAL ECOSYSTEMS
• Reduced photosynthesis from light scattering
• Aluminum soil toxicity inhibits root growth
• Nitrogen over-fertilization alters plant competition
• Increased tree mortality from acid stress
🌊 AQUATIC SYSTEMS
• Acidification of lakes and streams
• Aluminum mobilization damages fish gills
• Collapse of plankton food webs
• Long-term biodiversity loss
VII. IRREVERSIBILITY & GOVERNANCE RISKS
A. Termination Shock
If aerosol spraying stops suddenly:
• Rapid temperature rebound
• Ecosystems and agriculture unable to adapt
• Severe weather acceleration
B. Scientific Uncertainty
• No full-scale controlled experiments possible
• Feedback loops poorly understood
• Regional impacts unequal and unpredictable
C. Ethical & Legal Risks
• Cross-border climate effects without consent
• Disproportionate harm to vulnerable populations
• No established liability or remediation mechanisms
IX. CONSOLIDATED RISK MATRIX
X. SCIENCE OPERATIONS (SCI-OP)
Human Psychology and Behaviour
In addition to being a source of information, this article also serves as an exercise in human psychology and behaviour. Most people will form an opinion about the information in this article after the first few sentences and they will either stop reading and leave, or submit a comment, even though they really have no idea what the details are actually about.
This article is not a hypothetical geoengineering project. This article is about microscopic air pollution caused by global aviation and rocketry.
This article is an example that exposes the method by which globalist organizations (and others) present overwhelming amounts of pseudo-scientific information in a format that causes the reader’s minds to jump to conclusions before they have taken the time to fully comprehend the information.
This article presents details about the real-life, ongoing “experiment” of global aviation and rocketry that is thoughtlessly poisoning our atmosphere and planet. It is also designed to help readers comprehend how Sci-ops (as opposed to Psy-ops) are used to manipulate your mind.
All of the harms listed in this article are real. This is what invisible, microscopic air pollution from global aviation and rocketry is actually doing to each and every one of us, everyday, everywhere.
I realize that you may still be confused. If you would like to learn more about this issue and you are unable to wait for my upcoming article with all the details, then feel free to contact me directly at 310-619-3055 via phone, text, Signal, Telegram or WhatsApp.
This article clearly violates the advice presented below but that is because this article is NOT designed to convince anyone who does not want to be convinced.
This article contains far too much data, facts, evidence and information that clearly conflict with the prevailing narrative to which most people subscribe.
This article IS written for those rare people (approximately 1 out of 10,000) who rely on verifiable facts and legitimate evidence to inform their views.
This article IS designed to be an ENORMOUS resource of information, data, facts and evidence for those rare people who value such things.
How many times have you heard that the white lines in the sky are the result of an evil cabal that is operating a covert spraying operation (which is nevertheless clearly visible) and that the problem is NOT caused by jet fuel.
Have you been told that “THEY” are spraying you with strontium, aluminum and barium? CLICK HERE
If you still believe that you are being “sprayed,” maybe you ought to read this article at least two more times.
If you would like to have a respectful discussion regarding this issue and help work on possible solutions, then please feel free to contact me directly anytime at 310-619-3055 (phone, text, Signal, Telegram or WhatsApp) or James.Roguski@gmail.com
James Roguski
310-619-3055
My Story
JamesRoguski.substack.com/archive
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See Dane Wigington's website: Geoengineering.org.
However, I don't believe that most geoengineers are actually unwitting. I believe that many, if not most, know exactly what they are doing.
Blessings and appreciation from Sydney Australia.