C5 - Role of Soils in Waste Management Flashcards

1
Q

is heterogeneous material made up of three major
components: a solid phase, a liquid phase, and a gaseous
phase.

A

soil

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2
Q

three phases that influence the supply of
plant nutrients to the plant root

A

solid phase, liquid phase, gaseous
phase

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3
Q

the main nutrient reservoir

A

solid phase

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4
Q

holds nutrients in the cation form (positive charged
ions), such as potassium, nitrogen (as ammonium),
sodium, calcium, magnesium, iron, manganese, zinc,
and cobalt on negatively charged clay and organic
colloidal particles

A

solid phase

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5
Q

held very loosely to the anion exchange sites
of the soil and move readily with percolating soil
water

A

nitrate

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6
Q

is often fixed to the mineral soil fraction
containing iron, aluminum, and carbonates

A

phosphorus

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7
Q

The amount of plant available nutrients held by a soil
depends upon its unique ______

A

chemical and physical makeup

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8
Q

is responsible for the transport of nutrients in the soil

A

liquid phase

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9
Q

large percentage of agricultural waste material is composed
of __

A

water

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10
Q

mediates the exchange of gases
that occurs among the numerous living organisms in
the soil

A

gaseous phase

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11
Q

used to deplete Biological
Oxygen Demand (BOD), consume or remove such
biostimulants as phosphates and nitrates, provide long
term storage of heavy metals, and deactivate pathogens
and pesticides

A

soil filtering

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12
Q

Soil factors that affect biological degradation

A

temperature
moisture
oxygen supply
pH
available
nutrients (N, P, K, and micronutrients)
porosity
permeability
microbial population
bulk density

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13
Q

is primarily controlled by the chemical and biological composition of the waste material, soil moisture and temperature, and available oxygen supply

A

decomposition rate of organic material

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14
Q

soil-agricultural waste interaction

A

filtration
biological degradation
chemical reactions

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15
Q

Organic waste mineralization by-products consist of __

A

macro- and micro-plant nutrients, soluble salts, gases,
and heavy metals

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16
Q

is the replacement or interchange of ions bonded
electrostatically to exchange sites on soil particles and soil organic materials with similarly charged ions in
the soil solution

A

Ionic exchange and adsorption

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17
Q

is the adsorption and exchange of
nonmetal and metal cations to negatively charged sites
on soil particles and soil organic materials

A

cation exchange

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18
Q

is the measure of a soil’s
potential to exchange cations and is related to soil
mineralogy, pH, and organic matter content

A

Cation-exchange
capacity (CEC)

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19
Q

is the exchange and replacement of
negatively charged ions to positively charged sites on
soil particles.

A

anion exchange

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20
Q

is relatively low in most soils when compared to cation exchange; however, anion exchange is important because the
anion exchange potential of the soil is related to its
ability to retain and exchange nitrate nitrogen
(NO3–N), sulfate, chloride, boron, molybdenum, and
phosphorus.

A

Anion exchange capacity

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21
Q

are processes that remove an ion from the soil solution

A

Adsorption and precipitation

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22
Q

occurs as ions attach to the solid soil surface through weak
chemical and molecular bonds or as strong chemical
bonds.

A

Sorption

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23
Q

is the deposition of soluble
compounds in soil voids. It occurs when the amount of
the dissolved compounds in the soil solution exceeds
the solubility of those compounds.

A

precipitation

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24
Q

is the interaction of metals with soil
organic matter and some oxides and carbonates,
resulting in the formation of large, stable molecules.

A

complexation

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25
is a process where microbes digest organic waste, reduce the waste material to inorganic constituents, and convert it to more stable organic materials
Organic waste mineralization
26
released during this process are the essential plant nutrient (N, P, K), macronutrients and micronutrients, salts, and heavy metals.
inorganic materials
27
is converted to inorganic nitrogen and made available for plant growth during the waste mineralization process.
organic nitrogen
28
is the initial by-product of organic nitrogen mineralization
Ammonium nitrogen (NH4+)
29
can contaminate if leached below the soil root zone or transported off the field by runoff to surface water.
nitrate
30
is removed from the soil solution by adsorption to the surface of clay particles or complexation with carbonates, iron, aluminum, or more stable organic compounds.
phosphorus
31
is dependent on the phosphorus adsorption and complexation capacity of a soil.
Phosphorus mobility
32
is considered unavailable for plant growth
Adsorbed phosphorus
33
Potassium, calcium, and magnesium converted from organic to inorganic compounds during ____ have similar reactions in the soil.
mineralization
34
is less mobile than nitrogen and more mobile than phosphorus.
potassium
35
are by-products of the organic mineralization process. Municipal sludge applied on the land is often a source of heavy metals.
Heavy metals and trace elements
36
Soil-agricultural waste mineralization relationship
microbial activity nitrogen mineralization phosphate mineralization potassium, calcium, and magnesium mineralization heavy metal and trace element mineralization
37
is the rating given soils that have properties favorable for the use of agricultural wastes. The degree of limitation is minor and can be overcome easily. Good performance and low maintenance can be expected.
slight
38
are needed to determine and document site specific soil information, such as soil type, observed and inferred soil properties, and the soil limitations or hazards for the site specific components.
soil investigations
39
is a measure of the soil’s capacity to hold water in a form available to plants. It is a function of soil porosity, texture, structure, organic matter content, and salinity.
Available water capacity
40
is generally expressed as the sum of available water in inches to a specified soil depth
Available water capacity
41
is expressed in grams per cubic centimeter. It affects infiltration, permeability, and available water capacity
bulk density
42
is an index of the soil’s capacity to exchange cations with the soil solution. It affects the ability of the soil to adsorb and retain cations and heavy metals.
Cation-exchange capacity (CEC)
43
is the depth from the soil surface to soft or hard consolidated rock or a continuous indurated or strongly cemented pan
depth to bedrock or a cemented pan
44
is the highest average depth from the soil surface to the zone of saturation during the wettest period of the year. This saturated zone must be more than 6 inches thick and persist for more than a few weeks.
Depth to high water table
45
is the temporary covering of the soil surface by flowing water.
flooding
46
are the soil fractions greater than 3 inches and are measured as a weight percent or estimated as a volume percentage of the whole soil
Rock fragments, stones, and boulders
47
is a soil surface feature that is defined as the percent of stones and boulders (rock fragments greater than 10 inches in diameter) that cover the soil surface.
Stoniness
48
is the rate at which water enters the soil surface.
intake rate
49
is the quality of soil that enables water to move downward through the soil profile.
permeability rate
50
affects plant nutrient availability, agricultural waste decomposition rates, and adsorption of heavy metals.
soil pH
51
is standing water in a closed depression that is removed only by percolation, transpiration, or evaporation.
ponding
52
is the concentration of dissolved salts in the soil solution and is related to electric conductivity
salinity
53
is the standard measure of soil salinity and is recorded as Mmhos/cm.
electrical conductivity
54
interferes with the ability of the plant to absorb water from the soil and to exchange plant nutrients.
high soil salinity
55
is the inclination of the soil surface from the horizontal expressed as a percentage
slope
56
slope influences __ with which machinery can be used
runoff velocity, erosion, and the ease
57
is represented by the Sodium Adsorption Ratio (SAR), which is the measured amount of sodium relative to calcium and magnesium in a water extract from a saturated soil paste
sodium adsorption
58
Droughty: recommendations and impact if degree of limitation is slight (>6 in)
apply waste; improves available water capacity
59
Droughty: DOL is moderate. 3-6 in
reduce application rates; improves available water capacity. contaminants can flow into the ground
60
Droughty: severe; < 3.0 in
reduce application rates and use split applications
61
dense layer (bulk density) soil texture: medium and fine coarse <1.7, slight
apply when soil moisture contents is such that the field is in tillable condition
62
Low adsorption: slight, >15
apply waste
63
Low adsorption: moderate 5-15
reduce application rates
64
Low adsorption: severe
reduce application rates
65
BASAHA ANG TABLEE KAY TAAS KAAYO HAHSHAHSAHSH
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