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Which factors impact adsorption/desorption and precipitation/dissolution
adsorption/desorption: pH, clay content, amt of soil Ca, Fe, and Al.
precipitation/dissolution: pH and the concentrations of soil Ca, Fe, and Al.
Explain the difference between enzymatic hydrolysis and biological solubilization
Enzymatic hydrolysis uses enzymes such as phosphatases to release P from organic compounds.
Biological solubilization uses organic acid anions to bind Ca, Fe, or Al and release P from phosphate minerals.
how and why P availability is affected by total soil P content:
It sets the size of the potential P supply, but only a small share is in solution and readily available. A soil can contain a lot of total P while having little immediately available P.
how and why P availability is affected by Ca, Fe, Al concentrations:
They can bind P in secondary minerals or on mineral surfaces. This reduces solution P; how strongly it happens depends on soil conditions such as pH.
how and why P availability is affected by pH:
In acidic (low pH) soils, P can be strongly associated with Fe and Al oxides; Ca phosphates are also affected by pH.
how and why P availability is affected by Contact of soil solution to soil minerals and roots:
P moves through soil mainly by slow diffusion. Roots need to encounter P in the soil solution, or reach nearby P that can be released from minerals or colloids.
how and why P availability is affected by temperature:
Temperature influences weathering and biological activity, which can affect how quickly P is released and cycled. The slides list temperature as a factor but do not specify a numerical effect.
how and why P availability is affected by clay type/types of colloids:
Clays and Fe/Al oxides provide surface area and sites that can adsorb P. Some Fe/Al oxides also have tiny pores that can trap P, making it less available.
List 4 ideas to increase P availability for your crop, based on our understanding of the physicochemical processes governing P cycling
Root exudates containing organic anions to bind Ca, Fe, and Al to release O
Use phosphates to release P from OM
Mycorrhizal associations
Improve root architecture
List advantages and limitations of the Olsen P test
Advantage: practical soil-test estimate that can be related to crop yield response and fertilizer need
Limitation: it is an estimate and P is very variable
Explain the difference between root foraging, P mining, and increasing P use efficiency
Root foraging: helps plants find P with less soil
P mining: release P from minerals or OM using educates/enzymes
P use efficiency: producing more growth or yield for each unit of P the plant takes up.
What is phosphatase?
An enzyme that helps break down organic P compounds, releasing inorganic P that plants can take up.
How is K availability affected by CEC, SOM, texture, and clay type?
High CEC = Hold More K
Texture and Clay amt influence CEC = amt K held
More SOM = High CEC = Hold More K
2:1 clays can also fix K between layers
Compare and contrast which concepts, pools and processes are similar or different between the N, P and K cycle

What are the dominant forms and distribution of S in the soil profile of a mollisol, spodosol, oxisol. Explain the observe patterns!
Mollisol: organic S is concentrated near the surface and declines with depth, inorganic S increases with depth
Spodisols: High amounts of organic S in soil surface and subsurface, very little inorganic s
Oxisols: inorganic S dominates and increases with depth in the diagram. More organic S on the top and decreases
How does pH affect calcium availability:
Acid soils generally have less Ca. Above about pH 7.2, additional Ca may form nearly insoluble compounds, including with P. Lowering pH can dissolve Ca in some secondary minerals.
List 2 potential challenges related to magnesium management.
Ca:Mg balance ( add gypsum when too low)
Mg and K imbalances ( causes cow illnesses)
What is the role of Magnesium in the plant?
A big part of the chlorophyll molecule and is involved in protein formation, ATP rxns, and enzyme activations.
Give 3 examples of plant management strategies and 3 examples of soil management strategies to increase micronutrient availability.
Plant strategies: rotate crops to support mycorrhizae; select crops or varieties with effective root uptake; support root–microbe partnerships.
Soil strategies: apply the needed micronutrient fertilizer; manage soil pH; use chelated nutrient sources where appropriate.
How does CEC affect calcium availability
High-CEC soils can hold more Ca; low-CEC soils hold less.
How does Cation saturation affect calcium availability
High levels or applications of other cations can reduce Ca uptake, especially when soil Ca is low to moderate.
How does Parent material affect calcium availability
How does Moisture affect calcium availability