A general soil spatial scaling theory

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Soil diversity is crucial for maintenance of sustainable ecosystems. Soil varies on a continuum from microbial habitats to fields, regions, continents and the globe. This project will take a unifying approach to derive a general spatial scaling theory that will allow us to estimate the likely behaviour of soil properties at all scales. Understanding the scaling behaviour of soil means one can be certain about describing the changes in relationships between soil properties and processes. It will enhance the ability to monitor soil property changes through time, essential for gauging effects of climate change and achieving food security.