In plants, the passing of a compound from one system into another such as water movement from soil into plant roots. In soils, the binding of a chemical into a soil particle.
Physical and physiological processes that prepare plants for temperature extremes.
In irrigation systems, adding of acidic materials such as sulfur or phosphoric acid to irrigation water with excessive pH, bicarbonate, and carbonate contents. This lowers the pH and converts bicarbonate and carbonate into carbon dioxide and water.
Aerated sludge that is subjected to bacterial processes.
Acidity of a soil solution from free hydrogen ions measured as pH.
Measurement (index) of the proportion of hot water soluble nitrogen (HWSN) relative to hot water insoluble nitrogen (HWIN) in urea formaldehyde fertilizers.
Molecular attraction and contact between the surfaces of two unlike substances or objects.
Bonding or adhering of ions or compounds to the surface of soil particles or plant parts.
In turfgrass, a method of cultivation where hollow or solid tines are inserted into and removed from the turfgrass and soil to control soil compaction and increase water and air penetration. Hollow tine aerificaiton involves using hollow tines that remove soil cores or plugs while solid tine aerification using solid tines and does not remove any soil.
Requiring oxygen or having oxygen present in the environment.
Collected together in tufts, groups, or bunches.
Soil that has a pH above 7.0.
The capacity of water to neutralize acids. A property imparted by carbonates, bicarbonates, hydroxides, and others.
Any material such as sand, sawdust, gypsum, diatomaceous earth, peat, or calcined clay that is added to soil to alter its chemical and/or physical characteristics.
Nitrogen containing organic acids that are building blocks to form proteins. Amino acids contain one or more amino (-NH2) groups, a carboxyl group (-COOH), and possibly sulfur.
Conversion of amino acids and other nitrogen containing organic compounds into ammonia (NH3) and ammonium ions (NH4+).
Not requiring oxygen or the absence of oxygen in the environment.
Weight of an atom of an element relative to the weight of an atom of carbon (12C), which has been assigned the value of 12.
Portion of soil water that can be readily absorbed by plant roots. Often considered to be that water held in the soil against a pressure of -33 kPa to approximately -1,500 kPa (or -15 bars).
Microscopic, single cell, non-green organisms with rigid cell walls that reproduce by cell division. Bacteria are prokaryotes.
The degree to which the cation exchange capacity’s binding or exchange sites are occupied with cations such as calcium, magnesium, sodium, and potassium as opposed to acid cations such as aluminum and hydrogen is referred to as the base saturation of a soil. Soil pH and fertility generally increase as the percentage base saturation increases.
Breakdown (digestion) by biological organisms.
The ability of a soil to resist chemical changes. The major buffering system for soils is the cation exchange capacity.
Measurement of soil compaction expressed as a weight per unit of soil (grams per 100 cc).
A granular soil modification amendment consisting of highly fired clay minerals such as montmorillinite and attapulgite clays that are absorbent and stable.
Plant food sources including sugars and starches containing carbon with hydrogen and oxygen in a 2 to 1 ratio, as in water (H2O).
Ratio of organic carbon weight to total nitrogen weight in soil or organic material.
Cation Exchange Capacity
Sum of exchangeable cations a soil can adsorb and retain against leaching and is expressed as centimoles per kg of soil or milliequivalent per 100 grams of soil. Sometimes referred to as the
Machine that spreads granules as they drop onto a spinning disc or blade beneath the hopper.
Cyclic structures of a normally non-soluble metal ion and an organic component that, when held together, become soluble in water.
Yellowing of normally green plant tissue due to chlorophyll loss.
Water Insoluble Nitrogen (WIN)
Insoluble nitrogen fertilizer fractions associated with urea reaction fertilizers that are insoluble in cold water (72 F).
Water Soluble Nitrogen (WSN)
Soluble nitrogen fertilizer fractions associated with urea reaction fertilizers that are soluble in cold water (72 F).
Very small particles that are formed during the weathering process of soils.
Residues from organic matter and soil piles allowed to undergo biological decomposition.
A meristematic growing point at or just below the ground where stems and roots join and new shoots emerge.
The disturbance of soil and/or thatch layer without destroying the turfgrass (e.g. aerification, slicing, spiking, etc.).
The biological conversion of nitrate or nitrite to gaseous nitrogen as either N2 or N2O.
Removal of excessive turfgrass thatch and/or mat using stiff rakes or a series of vertically mounted knives or tines.
Geological deposit of siliceous skeleton material of diatoms (algae).
Partially or completely treated waste water from a treatment plant, reservoir, or basin.
Electrical Conductivity (EC)
A measure of salinity using electrical conductance expressed millimhos per centimeter (mmhos/cm) or decisiemens per meter (dS/m).
A negatively charged subatomic particle which orbits the atom’s positively charged nucleus, determining the atom’s chemical properties.
A substance composed of only one kind of atom. These combine to compose all materials.
A complex organic agent that enhances cellular reaction rates without being altered in the process.
Exchangeable Sodium Percentage (ESP)
A measure of excessive sodium hazard in the soil as the ratio (as percent) of exchangeable sodium to the remaining exchangeable cations (Ca, Mg, and K).
Fertilizing through irrigation systems.
Any material, except lime, supplying essential nutrients to plants.
Plant injury from dehydration due to contact with materials containing salts.
The percentage of water a soil retains against the action of gravity and typically is that remaining in a soil 2 to 3 days after having been saturated and free drainage has occurred. Estimated at -33 kPa water potential.
Light liquid fertilizer applications to plant foliage.
Subsurface water in the zone of saturation that moves freely, often horizontal.
Metals with densities of 5 mg per meter or greater and include Cd, Co, Cr, Cu, Fe, Hg, Mn, Mo, Pb, and Zn.
Hot Water Insoluble Nitrogen (HWIN)
Insoluble nitrogen fertilizer fraction associated with urea reaction fertilizers that is insoluble in hot water (212 F).
Portion of soil organic matter that is insoluble in dilute alkali.
Portion of humus that is water insoluble and is extracted from soil with dilute alkali and precipitated upon acidification.
Relatively stable, dark-colored colloidal soil organic matter containing no recognizable plant parts.
Rate of water flow in soil as imposed by a hydraulic head.
Splitting of one molecule by addition of water.
Conversion of an element from the inorganic form to the organic form in microbial or plant tissues. Often used to describe the conversion of nitrate or ammonium into organic forms by soil microorganisms.
Downward movement or entry of water into the soil.
Electrically charged atoms resulting from the loss of electrons (cations) or gain of electrons (anions).
Downward movement of soluble materials through a soil.
Calcium oxide (CaO) and/or a variety of acid neutralizing materials containing Ca, Mg, or both Ca and Mg.
Sedimentary rock composing more than half calcium carbonate (CaCO3).
Applying nutrients as dissolved fertilizer in solution.
Nutrients needed in largest amounts (usually 50 mg/kg) for plant growth (e.g. C, N, O, K, Ca, Mg S, and H).
Elements or nutrients needed in only small amounts (usually less than 50 mg/kg) for plant growth (e.g. B, Cl, Cu, Fe, Mn, and Zn).
Conversion o fan organic form of an element to an inorganic form (e.g. conversion of organic nitrogen to ammonium nitrogen) by microbial decomposition.
Microbial oxidation of ammonium nitrogen to nitrites and eventually to nitrates.
Residual decomposition of plant or animal content in soil.
Diffusion of water or any solvent (pure liquid) from a region of greater water potential to one of lesser water potential across a selectively permeable membrane.
Loss of an electron by an atom or molecule where oxygen is the electron acceptor.
Partially decomposed organic matter accumulating under wet conditions.
Downward movement of water through a soil profile.
Degree of acidity or alkalinity. Defined as the negative logarithm of hydrogen ion activity. A scale of 0 to 14 is used where 7 is neutral, below 7 is acidic and above 7 is alkaline.
Sewage Sludge / Bio-Solids
Settled sewage solids removed by screening, sedimentation, chemical precipitation, or bacterial digestion.
Upper layer of Earth’s surface used as the natural medium for plant growth.
A molecule dissolved in a solution.
Brown to black colored layer of dead turfgrass plant leaves, stems, rhizomes, crowns, and stolons between the green colored vegetation and the soil surface.