Use LEFT and RIGHT arrow keys to navigate between flashcards;
Use UP and DOWN arrow keys to flip the card;
H to show hint;
A reads text to speech;
42 Cards in this Set
- Front
- Back
Actinomycete |
Group of soil bacteria resembling fungi. Acitinomycetes play a role in the decomposition of organic matter and the release of mineral elements. |
|
aggregate |
(1) close cluster or mix of small particles of soil and/or organic matter of various sizes that are bonded together; and/or sand, gravel, or small rocks in soil; and/or sand, gravel, or small rocks used under paving surfaces. * (2) &(3) not pertaining to soil science |
|
Anion |
Ion that contains a negative charge, Contrast with Cation |
|
Buffering Capacity |
Ability of a soil to maintain its pH |
|
Bulk Density |
Mass of soil per unit volume. Often used as a measure of compaction. |
|
Capillary Water |
Water held in the capillary pores of the soil; much of this water cab move in any direction and is readily available to plants roots. |
|
Cation |
Positively charged ion.In soils the most abundant cations are Calcium (Ca), magnesium (Mg), Potassium (K), Sodium (Na), and Aluminum (Al). contrast with anion |
|
Cation Exchange Capacity (CEC) |
Ability of a soil to absorb and hold cations. Affected by soil pH. Measures soil fertility, clay composition, and engineering characteristics. |
|
Clay |
(1) Soil particles with a typical grain sixe of less then 0.004 mm. (2) Soil predominately composed of such particles. Contrast with Sand and Silt. |
|
Exudates |
Substance or solution that oozes out of injured plant cells or is secreted through membrane pores. |
|
Field Capacity |
Maximum soil moisture content following the drainage of water due to the force of gravity. *Compare to available water, gravitational water, and permanent wilting point. |
|
Gravitational Water |
Water that drains from the larger soil macropores due to the force of gravity. *Compare to available water, gravitational water, and permanent wilting point. |
|
Horizon |
Layer of soil within the soil profile. |
|
Humus |
dark colored, stable form of organic matter that remains after most of the plant or animal residues have decomposed. |
|
Ion |
atom or a group of atoms with a positive or negative charge. |
|
Leach(leaching) |
(1) tendency for elements or compounds to wash down through the soil. (2) tendency for elements or compounds to wash into the soil. For example, alkaline compounds may leach from concrete, or heavy metals may leach from aggravates, and both may do plant damage. |
|
Loam |
Soil texture classification based on a certain ratio of sand, silt, and clay. Considered Ideal for plant growth. |
|
Macropore |
relatively large space between soil particles that is usually air filled and allows for water movement and root penetration. *Contrast with Micropore |
|
Micropore |
space between soil particles that relatively small and likely to be water filled. *Contrast with Macropore |
|
Mineralization |
Process in which an organic substance is converted to or trapped in inorganic substance. |
|
Mycorrhizae |
Symbiotic association between some fungi and the roots of a plant. |
|
Nematode |
microscopic round worm.many are beneficial organisms, but some feed on plant tissues and may cause disease or damage. |
|
Nutrient Cycling |
Movement of mineral elements( sometimes called nutrients) within an ecosystem as organic matter decomposes releasing bound nutrients back to plants. |
|
Organic Layer |
Layer of organic matter at the soil surface |
|
Parent Material |
soil bedrock or base material from which a soil profile develops. |
|
Permanent wilting point |
Point at which a plant cannot pull anymore water from the soil and suffers permanent damage. |
|
pH |
Unit of measure that describes the alkalinity or acidity of a solution. Negative log of the hydrrogen ion concentration. Measured on a scale from 0 to 14. Greater than 7 is Alkaline, less then 7 is acid, and 7 is neutral (pure water) |
|
rizosphere |
soil area immediately adjacent to, and affected by, plant roots. Typically has a high level of microbial activity. |
|
saline soil |
Soil with a high concentration of soluable salts. Can cause poor plant growth. |
|
sand |
soil particles with a size between 0.06 and 2mm in diameter. *Contrast with clay and silt |
|
silt |
Soil particles with a grain size between 0.004 and 0.062 mm (coarser then clay particles but finer than sand). *contrast with clay and sand |
|
sodic soil |
soils with relatively low levels of soluble salts and a concentration of sodium high enough to adversely affect soil structure (symptoms include water logging, erosion, soil surface crusting, and poor plant growth) Soils >12 SAR (sodium absorption ratio) |
|
soil compaction |
Compression of the soil, often as a result of vehicle or heavy equipment traffic, that breaks down soil aggregates and reduces soil volume and total pore space, especially macro pore space. |
|
soil food web |
complex network of interconnected food chains in an ecosystem; in this case, in the soil. |
|
soil profile |
vertical section through the soil and all of the soil horizons. |
|
soil structure |
arrangement of soil particles into aggregates |
|
soil texture |
relative fineness or coarseness of a soil due to particle size (sand, silt, and clay) |
|
structural cells |
Modular system consisting of units of soil and integrated support structures that serve as both a foundation for paved surfaces and a hospitable environment for tree root growth. |
|
structural soil |
Pavement substrate that can be compacted to meet engineering specifications yet remains penetrateable by tree roots in the urban environment. composed of angular crushed stone, clay loam, and hydrogel mixed in a weight ratio of 100:20:0.03. Developed at the Urban Horticulture Institute, Cornell University, Ithica, NY |
|
suspended sidewalk |
Sidewalk that is reinforced and supported with piers or other structures so that it does not rely on compacted sub grade or soil for support. |
|
symbiotic |
association of two different types of living organisms that is often , but not always beneficial to each. |
|
water-holding capacity |
ability of a soil to hold moisture |