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Series showing strength of cation attraction relative to pH Al(3+)>Ca(2+)>Mg(2+)>K(+)=NH4(+)>Na(+) Strongest Held-----------Weakest Held |
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Shows how much moisture in soil expressed as a volume of water in a cubic meter(or cm) ((Vwater)/(Vsoil))x100 |
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Gravimetric Water Content |
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A measure of amount of water in a soil, based on mass. ((mass of wet soil)-(mass of dry soil))/(mass of dry soil) |
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Caused by waters attraction to other things causes water to rise against gravity h=(.15/r) |
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Measure of waters attraction to solid surfaces, always negative water moves from high energy (wet soil) to low (dry soil) if Pmatric=0 soil is saturated |
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Measure of potential of water to move due to gravity, based off some chosen reference point, usually lower so the potential is positive |
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Measure of the part of soil water potential that is affected by presence of solutes, more solutes = lower potential |
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Amount of water the soil will hold against gravity naturally (soak the soil then let excess drain off remaining is FC)usually -10<-33 kPa |
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Permanent Wilting Point (PWP) |
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Definition
PWP is the point at which water is held so tightly to clay surfaces plants can no longer extract water and die <-1500kPa |
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The point at which soil is physically not able to hold any more water (when Pmatric=0) 0kPa |
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Instrument used to measure soil water potential, consists of porous cup connected to vacuum doesn't let air in |
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Cations of LOWER charge may substitute for HIGHER charge cations during mineral formation, always - charge usually found in 2:1 layer silicates |
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Found in all clays,charge changes with soil pH low pH= + charge high pH= - charge |
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An organic or inorganic clay with a ratio of 1 octahedral and 1 tetrahedral layer this creates a very tight bond not letting much iso sub happen |
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Ratio of 2 tetrahedral and 1 octahedral layers, much more common with iso sub |
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Intense weathering, pH dependant charge Negative charge above 5-7 pH Positive charge below 5 pH No charge in 5-7 pH |
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Stable organic "residue" from breaksown of org matter, greatly affected CEC almost always - charge is pH above 3 |
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Definition
Things in between the layers in a crystalline structure (example K+ in between layers in Kaolinite) |
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Any particle with a high surface area/mass ratio and is less than .002 mm |
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Silicon Tetrahedral Layer |
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Definition
Combined with Al octahedral layer in 2:1 and 1:1 proportions to make crystalline structure looks like Si pyramids. |
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Aluminum Octahedral Layer |
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Definition
Combined with Si Tetrahedral layer in 2:1 and 1:1 proportions to make crystalline structure looks like 2 pyramids stacked base to base |
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Definition
Movement of gas particles due to concentration gradient, moves from more gas particles to less until all areas have equal ratios, much slower through water (explains organic buildup in histosols) |
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movement of gasses due to differences in pressure, not as important as diffusion |
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Soils that have been exposed to anaerobic conditions for long time (waterlogged histosols) may have switched to anaerobic respiration using N2 |
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Measure of total Neg charge available to attract + cations Low CEC=highly weathered= not much - charge High CEC=2:1 Silicates or Organic Matter (Humus) |
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The ability of soil to resist a pH change, determined by colloidal fraction (clay%) and CEC |
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A reaction involving reduction (gain electrons reduce charge) and oxidation (lose electrons gain charge) |
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The proportion of soil mass over soil volume |
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The percent of space taken up by soil pores =100-((Bulk density)/(Particle density or 2.65g/cm^3))*100 |
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Plant Available Water (PAW) |
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Definition
FC-PWP=PAW the amount of water held naturally - permanent wilting point = plant avail water |
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Definition
The amount of light reflected by a soil ranges from .1(dark colored soil) to .5(light) |
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Basic formula for all life (Sugar+Water+Oxygen)=(Water energy and carbon dioxide) |
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Measure of tendency of something to become oxidized or reduced (tendency of electrons to move) |
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A 1:1 Silicate clay, very stable and nonreactive,little-no weathering, H bonding makes bond too tight for iso sub, very low CEC, small pH charge |
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A 2:1 layer silicate clay, more weathered than illite, iso sub in Tetra sheet, High CEC |
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2nd level weathering, more than kaolinite, iso sub in tetra sheet, medium CEC, K+ in inter-layers binds layers together preventing swelling |
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Montmorillionite (Smectite) |
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Definition
Very expandable 2:1 layer silicate, most weathered, a lot of iso sub and high CEC |
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