m (→Phosphorus) |
m (→Phosphorus) |
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*Soil pH: Optimum soil pH between 6 and 7 will result in maximum phosphorus availability. At low pH (acidic soils), soils have greater amounts of aluminum and iron, which form very strong bonds with phosphate. At high pH phosphate tends to precipitate with calcium. | *Soil pH: Optimum soil pH between 6 and 7 will result in maximum phosphorus availability. At low pH (acidic soils), soils have greater amounts of aluminum and iron, which form very strong bonds with phosphate. At high pH phosphate tends to precipitate with calcium. | ||
*Temperature, moisture, and soil aeration can affect the rate of P mineralization from organic matter decomposition. | *Temperature, moisture, and soil aeration can affect the rate of P mineralization from organic matter decomposition. | ||
+ | |||
+ | '''Additional reading''' | ||
+ | *[https://www.aces.edu/blog/topics/crop-production/understanding-phosphorus-forms-and-their-cycling-in-the-soil/ Phosphorus Basics: Understanding Phosphorus Forms and Their Cycling in the Soil] | ||
+ | *[https://extension.umn.edu/phosphorus-and-potassium/understanding-phosphorus-minnesota-soils Understanding phosphorus in Minnesota soils] | ||
+ | *[https://cropwatch.unl.edu/documents/USDA_NRCS_phosphorus_guide.pdf Soil phosphorus] - USDA-NRCS | ||
+ | *[https://www.ctahr.hawaii.edu/mauisoil/c_nutrients02.aspx Phosphorus] | ||
+ | *[https://www.croplife.com/crop-inputs/how-to-effectively-manage-phosphorus-levels-in-the-soil/ How to Effectively Manage Phosphorus Levels in the Soil] | ||
+ | *[https://stormwater.pca.state.mn.us/index.php?title=Phosphorus Phosphorus] - information in this manual on phosphorus in stormwater | ||
===Nitrogen=== | ===Nitrogen=== |
Overview of soil physical properties and associated activities affecting soil physical properties and processes. Click on links to go to a specific section. | ||||
Property | Effects | Desired value | Management strategies | |
Phosphorus | ||||
Nitrogen | ||||
Major cations | ||||
Sulfur | ||||
Trace metals | ||||
Cation exchange capacity | ||||
Electrical conductivity | ||||
Organic matter (carbon) | ||||
Base saturation | ||||
Enzymes | ||||
Salinity | ||||
Sodium adsorption ratio | ||||
pH |
Soil chemical properties include concentrations of specific chemicals (e.g. phosphorus, nitrogen, carbon, major cations (calcium, magnesium, sodium, potassium), sulfur, trace metals and elements), pH, cation exchange capacity, base saturation, salinity, sodium adsorption ratio, enzymes, and electrical conductivity. These properties affect processes such as nutrient cycling, biologic activity, soil formation, pollutant fate, and erosion.
This page provides an overview of soil chemical properties, processes they affect, effects of human activities, discussion of stormwater applications, and links to related topics, including information on sampling, testing, and soil health assessments.
Soil chemical properties discussed below include phosphorus, nitrogen, major cations, trace metals, cation exchange capacity, electrical conductivity, enzymes, organic matter and carbon, base saturation, salinity, sodium adsorption ration, and pH.
Phosphorus constitutes about 0.2 percent of a plant’s dry weight, where it is primarily a component of tissue molecules such as nucleic acids, phospholipids, and adenosine triphosphate (ATP). Along with nitrogen, phosphorus is often a limiting nutrient in soil. Soils limited in phosphorus reduce plant growth and development, while excess phosphorus can be exported from soil and enter freshwater bodies.
Approximately 30 to 65 percent of total soil phosphorus is in organic forms and the remaining 35 to 70 percent in inorganic forms. Soil microorganisms play a key role in processing and transforming organic forms into plant available forms. Inorganic phosphorus forms include the following:
Phosphorus is typically measured in a laboratory with one of the following methods.
Phosphorus can also be determined in the field with appropriate equipment or with test strips. Test strips are less accurate but may be suitable for identifying phosphorus deficiencies.
The soil phosphorus cycle is somewhat complicated since phosphorus is affected by soil mineralogy and chemistry and by soil biotic processes.
Additional reading