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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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Definition
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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Definition
Stable organic "residue" from breaksown of org matter, greatly affected CEC almost always - charge is pH above 3 |
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| 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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| 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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| 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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