pH |
Controls nutrient availability, influences microbial communities, and soil processes |
A soil pH of 5.5–7 is ideal for most crops to obtain necessary nutrients |
POXC |
Measure of reactive carbon pool readily accessible to microbes and is very strongly correlated with other indicators of soil health like total organic C (TOC)62
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Soil carbon pools are important for maintaining soil function imperative to plant growth, shown to affect agronomic performance63
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Carbon fractions |
Changes in soil organic carbon (SOC) require decades. C fractionation can show faster changes (Particulate organic matter- POM) as well as indicate the stability of the soil C (mineral-associated organic matter- MAOM). POM also plays roles in soil aggregation and infiltration |
POM is primary source of plant available N. SOC is important for controlling soil functions (e.g. water and nutrient regulation) imperative for plant growth |
Water infiltration |
The amount of water able to move though soil and is related to soil compaction, pore space, and water retention abilities |
Important component of plant water availability and compaction affecting root growth |
Microbial abundance |
Microbes are the base of the trophic chain and important players in decomposition, nutrient availability, and C storage |
Plants benefit from easily available nutrients, increased SOC, and improved soil structure supported by microbial processes. Increased microbial diversity has been linked to plant health and growth64
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Microbial diversity |
Higher microbial functional diversity can support more soil processes and healthier soils65
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