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Terry Marsh, senior hydrologist at the CEH, said: "Late May soils were the driest on record across large parts of eastern and central England, causing substantial agricultural stress [and] impacting on crop yields.
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In addition, their direct release onto soil may affect soil's physical and chemical properties including soil porosity and pH (Niaounakis and Halvadakis 2006; Mekki et al. 2013).
Effective management by adding straw and polyacrylamide (PAM), i.e., SPAM, to soil may increase soil stability, including structure and fertility.
The shallower root distribution and soil biological crusts may reduce soil desertification trends and improve soil porosity, thereby decreasing the soil bulk density.
Soil fauna may affect soil organic matter (SOM) dynamics not only by assimilating litter but also by modifying the soil environment at many spatiotemporal scales.
Applying water-absorbing soil amendment may improve soil structure, arise water storage and decrease other water-related limitations (Huettermann et al. 2009).
There is concern that whole-tree harvesting may acidify soils and surface waters.
Rare earth elements (REEs) can be used to trace eroded soil sources but their efficacy may be soil dependent.
Likewise, differences and diversity in root morphology may allow soil biota to populate the soil profile more completely than in simply structured environments.
Finally, land cover change may affect soil moisture alternation toward different transformation directions.
Too much sand in the soil may make the soil dry, and too much clay may make it too wet.
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