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Atmosphere
layer of gas or layer of gases that envelop a planet and is held in place by the gravity of the planetary body
composed of about 78% nitrogen, 21% oxygen, and 1% of other gases.
Atmospheric Chemistry
study if the chemical process that occur in the Earth’s atmosphere and other planetary atmosphere
Layers of the Earth’s Atmosphere
Exosphere
Thermosphere
Mesosphere
Stratosphere
Troposphere
Composition of Air
a mixture of gases which makes up the Earth’s atmosphere
Common Properties of Air
Colorless and Odorless
Occupy Space
Air Exerts Pressure
Expansion
Colorless and Odorless
has no color and odor, an invisible matter that can only be felt
Occupy Space
mixture of gases, occupies space
Air Exerts Pressure
has weight and pressure exerted by the weight of air known as AIR PRESSURE
Expansion
on heating it expands and occupies more space. The more it expand the thinner it becomes. Hence the pressure of the warm wind is lower than that of cold wind
Chemical Reaction in Atmosphere
process in which various chemical substances in Earth’s atmosphere interact and transform into different compounds
Different Chemical Reaction in Atmosphere
Combustion Reaction
Ozone Formation
Photochemical Smog Formation
Acid Rain Formation
Aerosol Formation
Greenhouse Gas Reaction
Nitrogen Oxides (Nox) Formation
Volatile Organic Compounds (VOCs) Reaction
Hydroxyl Radicals (OH) Reactions
Nitrogen Fixation
Combustion Reaction
substance burns in oxygen with the release of carbon dioxide, water and energy in the form of heat, light and even sound.
Ozone Formation
formed in the atmosphere through the series of reactions involving oxygen molecules and sunlight
Photochemical Smog Formation
mixture of pollutants that are formed when nitrogen oxides and volatile organic compounds react to sunlight
Acid Rain Formation
formed when pollutants, primarily sulfur dioxide, react with atmospheric moisture
type of rain that contains high level of acidic components, primarily sulfur acid and nitric acid
Aerosol Formation
“Aerosols” are tiny particles suspended in the atmosphere
Aerosols can be formed through various chemical reactions, including the oxidation of sulfur dioxide and nitrogen oxide to form sulfate and nitrate particles
Greenhouse Gas Reaction
“Greenhouse gas” are gases in the Earth’s atmosphere that trap heat
Nitrogen Oxides (Nox) Formation
Nitrogen oxides (Nox), including nitric oxide (NO) and nitrogen dioxide (NO2), are produced through combustion process.
These gases are involved in reactions that contribute to the formation of photochemical smog.
Can also participate in the formation of acid rain.
Both NO and NO2 are formed during high-temperature combustion in the atmosphere, when oxygen combines with nitrogen.
Volatile Organic Compounds (VOCs) Reaction
“Volatile organic compounds” are organic compounds that have a high vapor pressure at room temperature.
High vapor pressure correlates with a low boiling point, which relates to the number of the sample’s molecules in the surrounding air, a trait knows as “valatility”
Hydroxyl Radicals (OH) Reactions
highly reactivate molecules present in the atmosphere
removing pollutants from the atmosphere
non-toxic to humans, animals, and plants
kills bacteria, virus and mold
4 Types of Hydroxyl Radicals
Atmospheric
In-vivo
Chemical
Interstellar
Nitrogen Fixation
vital process in which atmospheric nitrogen is converted into biologically useful forms, such as ammonia and nitrates
essential for the availability of nitrogen in ecosystems and the growth of plants
Challenges in Atmospheric and its impact to Agriculture
Climate Change
Air Pollution
Ozone Depletion
Acid Rain
Stratospheric Jet Stream
Space Weather
Aerosol Loading
Deforestation
Climate Change
refers to long-term shifts in temperatures and weather patterns, mainly caused by human activities especially burning of fossil fuels
Air Pollution
refers to contamination of the indoor outdoor environment by any chemical, physical or biological agent that modifies the natural characteristics of the atmosphere
Ozone Depletion
thinning of the ozone layer present in the upper atmosphere
Acid Rain
includes any form of precipitation with acidic components, such as sulfuric or nitric acid that fall to the ground from the atmosphere in wet or dry forms
Stratospheric Jet Stream
fast, narrow current of air flowing from the west to east that encircles the globe
Space Weather
refers to the variable conditions on the sun and in space
Aerosol Loading
suspensions of solids and/or liquid particles in the air that we breathe
Deforestation
removal of trees can disrupt the carbon cycle, affecting the atmosphere’s ability to absorb and store carbon dioxide.
Water
an inorganic compound with the chemical formula H20
transparent, tasteless, odorless, and nearly colorless chemical substance, and it is the main constituent of Earth’s hydrosphere and the fluids of all known living organisms
Bond
what holds atoms together in molecules
arise from the electrostatic forces between positively charged atomic nuclei and negatively charged electrons
Atom
smallest unit of matter; composed of three sub-atomic particles: proton, neutron, electron
Electron
negatively charged subatomic particle that can be either bound to an atom or free
together protons and electrons form an atom’s nucleus
Proton
subatomic particle with a positive electrical charge
found in every atomic nucleus of every element
Nuetron
have neutral electric charge and slightly more mass than positively charged protons
Molecule
group of atoms bonded together, representing the smallest fundamental unit of a chemical compound that can take part in a chemical reaction
Covalent Bond
sharing of electrons to form electron pairs between atoms
Hydrogen Bonding
Water Bond - consist of 1 atom of oxygen and 2 atoms of hydrogen
Properties of Water
Adhesion Force
Cohesion Force
Adhesion
joining two dissimilar substances is known as adhesion
force necessary for a liquid droplet to separate from a surface it comes into contact with is known as the adhesion force
Cohesion Force
defined as the force of attraction between two similar substances or molecules
The condition known as cohesive force describes how similar molecules are drawn to one another and stick to one another
Cohesion Force: Surface Tension
tendency to contract into the smallest possible surface area
Water has a very high surface tension because water is a polar molecule, its molecules are more attracted to one another than other molecules
Cohesion Force: Tensile Strength
maximum force per unit area that a continuous column of water can bear before breaking
Specific Heat Capacity
quantity of thermal energy required to increase a substance’s temperature by one degree Celsius per gram
Heat of Vaporization
amount of heat needed to change the state of a substance from a liquid to vapor. It is also known as the enthalpy of vaporization, with the amount of 4.07 × 10⁴ J/mol
Heat of Fusion
the energy required to change a substance from the solid state to the liquid state. Also known as, the enthalpy of heat of fusion, with the value of 6009.5 J/mol
Water Quality
Refers to the chemical, physical, and biological characteristics of water based on the standards of its usage
Dissolve Oxygen
also known as DO, is an oxygen dissolve in water
Two Types of Mixture
Solution
Suspension
Solution
homogeneous mixture composed of two or more substances
Solute
substance that is being dissolved
Solvent
dissolves the solute
Suspension
heterogeneous mixture in which the solid particles are spread throughout the liquid without dissolving in it
Two Ways of Oxygen Enters in Water
Atmosphere
Photosynthesis
What happen in the dissolved oxygen
It essential for the survival of fish and other aquatic organisms.
Oxygen dissolves in surface water due to the aerating action of winds.
Oxygen is also introduced into the water as a byproduct of aquatic plant photosynthesis
Electrical Conductivity
measure of the capability of the material to pass the flow of electric current
denoted by the Greek letter ρ
inverse of the resistivity and is given by σ = 1/ρ
pH Level
measures how acidic or basic a solution is
Formula: pH = - log [H3O+].
Alkalinity
the capability of water to neutralize acids This ability is referred to as a buffering capacity
measures how much acid can be added to a water body before a large pH change occurs
Hardness
measurement of the concentration of total divalent ions present in water
2 Types of Water Hardness
Temporary Hardness
Permanent Hardness
Temporary Hardness
occurs due to the presence of calcium hydrogencarbonate and magnesium hydrogencarbonate
can be removed by boiling water
Permanent Hardness
occurs due to the presence of calcium sulfate
cannot be removed by boiling water
Soil Chemistry
branch of soil science the deals with the chemical composition, chemical reactions and chemical properties in soils
Soil
dynamic living system in which ions and molecules constantly may move from one phase to the other, while ions and molecules constantly may move from one phase to the other, while interacting with each other
Soil chemical properties
based on the concentrations, and/or proportions of dissolved species in soil water and/or on the ion exchange complex
Soil Components
Inorganic Components
Organic Components
Inorganic Components
refer to the non-living materials present in the soil
primarily derived from the weathering and breakdown of rocks and minerals over time
Main Inorganic Components found in Soil
Mineral Particles
Rocks and minerals
Water and air
Mineral particles
primary inorganic components of soil, classified based on their size intro three categories: sand, silt, and clay
Rock and minerals
Soil contains various types of rocks and minerals, which contribute to its mineral composition
Water and air
While not strictly inorganic, water and air are crucial components of soil
Organic
refer to the living and decaying organisms, as well as their byproducts, that contribute to the fertility and structure of soil
Key Organic Components found in Soil
Humus
Plant Residue
Animal Residue
Micoorganisms
Humus
dark decomposed organic matter in soil
Plant Residue
Plant materials such as leaves, stems, roots, and fallen branches contribute to the organic component of soil
Animal Residue
Animal waste, carcasses, and other organic materials from animals also contribute to soil organic matter
Microorganisms
play a vital role in decomposing organic matter, cycling nutrients, and enhancing soil fertility
Soil Structure
refers to the aggregation of individual soil particles into compound groups orclusters of particles
Granular Structure
desirable soil structure characterized by the presence of small, rounded aggregates
Blocky Structure
consists of irregular, block-like aggregates
Prismatic structure
consists of vertical, column-like aggregates
Single-grained Structure
occurs when soil particles are not bound together and exist as separate particles
Massive Structure
refers to soil structure where soil particles are tightly packed together without any visible aggregation or distinct arrangement
Plate-like Structure
soil particles are arranged in thin, flat plates or sheets
Crumb structure
desirable type of soil structure characterized by the presence of small, loose and crumb-like aggregates
Plant Nutrients from Soil
Soil is a major source of nutrients needed by plants for growth. The three main nutrients are nitrogen (N), phosphorus (P) and potassium (K). Together they make up the trio known as NPK. Other important nutrients are calcium, magnesium and sulfur.
Two Main Categories of Nutrients
Macronutrients
Micronutrients
Macronutirents
required by plants in larger quantities
Soil pH significantly impacts the availability of macronutrients such as nitrogen (N), phosphorus (P), and potassium (K)
Nitrogen (N): In acidic soils, the availability of nitrogen increases, while alkaline soils can reduce nitrogen availability.
Phosphorus (P): Phosphorus availability decreases in alkaline soils due to the formation of insoluble compounds with calcium and iron
Potassium (K): Soil pH has a minimal effect on potassium availability. However, extremely acidic or alkaline conditions can reduce potassium uptake by plants
Micronutrients
needed in smaller amounts
Soil pH strongly influences the availability of micronutrients such as iron (Fe), manganese (Mn), zinc (Zn), copper (Cu), and boron (B)
Iron (Fe) and Manganese (Mn): Acidic soils promote the solubility and availability of iron and manganese, while alkaline conditions can lead to their precipitation, reducing their availability to plants
Zinc (Zn), Copper (Cu), and Boron (B): These micronutrients are more available in acidic soils. Alkaline conditions can cause their fixation or precipitation, rendering them less accessible to plants
Soil pH
refers to the measure of acidity or alkalinity of soil. It is a vital property of soil that affects the availability and uptake of essential nutrients by plants
determined by the concentration of hydrogen ions (H+) in the soil solution
plays a crucial role in the availability and uptake of nutrients by plants. It affects the chemical reactions and transformations that occur in the soil, which in turn influence nutrient availability
pH and Toxicity
pH measure of the acidity or alkalinity of a solution, ranging from 0 to 14.
A pH value of 7 is considered neutral, while values below 7 indicate acidity and values above 7 indicate alkalinity.
pH plays a crucial role in determining the toxicity of certain substances
Toxicity refers to the degree to which a substance can harm living organisms.
The pH of the environment can significantly influence the toxicity of certain substances
pH and Cation Exchange Capacity (CEC)
pH and cation exchange capacity (CEC) are both important concepts in soil science and agriculture
pH plays a crucial role in determining nutrient availability and microbial activity. Different plants have different pH requirements for optimal growth
CEC is a measure of a soil's ability to retain and exchange positively charged ions, known as cations. It is an important indicator of soil fertility and nutrient-holding capacity
Cation Exchange Capacity (CEC)
is a useful indicator of soil fertility because it shows the soil’s ability to supply three important plant nutrients: calcium, magnesium, and potassium
ph and Soil Organism
plays a significant role in determining the types and activities of soil organisms. Soil organisms, including bacteria, fungi, protozoa, nematodes, earthworms, and many others, are crucial for maintaining soil health and fertility
pH range 5.5–6.5 is optimal for plant growth as the availability of nutrients is optimal
Soil Acidity
Acidity in soil is primarily caused by the presence of hydrogen ions (H+). When certain minerals in the soil break down or when organic matter decomposes, they release hydrogen ions, which can increase soil acidity
Properties of Air
Air has mass
Air occupies space, or has volume
Air has density
Air exerts pressure
Chemistry of Water
Density is an important property of water because small changes in density result in a significant change in water pressure at great depths
Polarity means a molecule or bond has a separation of electric charge, creating a slightly positive end and a slightly negative end due to unequal sharing of electrons, determined by differences in electronegativity.
Cohesive Property means its molecules stick to each other due to strong hydrogen bonds, creating high surface tension (like water beading up or a needle floating) and enabling capillary action (water moving up xylem in plants), essential for life.