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World’s Soil Resources

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Figure 6.14: The soil’s hydraulic conductivity, K (cm day -1 ) in relation to the matric potential, ψ (MPa). As the matric potential becomes<br />

more negative the soil’s water content drops (see Figure 6.16) which increases the tortuosity and slows the flow of water. Source:<br />

Hunter College. 3<br />

The interactions between the structure and physical, chemical and biological components of the soil control<br />

the myriad soil functions and processes that are essential for healthy soils, ecosystems and human well-being.<br />

The soil acts as buffer and filter. Indeed, our soil is the world’s largest water filter. And through this buffering<br />

and filtering, soil controls the quantity and quality of the world’s liquid freshwater.<br />

6.10.2 | Quantifying soil moisture<br />

<strong>Soil</strong> water varies on multiple time and space scales, driven by climate, weather variability, land cover,<br />

topography and soil type and structure (Figure 6.15). Measuring variations in soil water is challenging especially<br />

at large scales where the cost of direct measurement would be very high. Long-term measurement networks<br />

have historically been limited to a few locations globally (Robock et al., 2000). However, with the recognition<br />

of soil water as an essential climate variable and the realization that in-situ measurements are necessary for<br />

the calibration and validation of remote sensing, the number of operational monitoring networks is increasing<br />

(Dorigo et al., 2011). There are also short-term experimental campaigns with multi-scale soil water sampling<br />

(Crow et al., 2012). For example, the <strong>Soil</strong> Climate Analysis Network (SCAN) in the United States provides soil<br />

water measurements for 174 sites across the United States, with some measurements dating back to 1992.<br />

New technologies such as the COsmic-ray <strong>Soil</strong> Moisture Observing System (COSMOS) cosmic-ray neutron<br />

probes (Zreda et al., 2012) have enabled more efficient and larger measurement footprints of the order of<br />

several hundreds of square meters.<br />

3 http://www.geo.hunter.cuny.edu/tbw/soils.veg/lecture.outlines/soils.chap.5/soils_chapter.5.htm<br />

Status of the <strong>World’s</strong> <strong>Soil</strong> <strong>Resources</strong> | Main Report Global soil status, processes and trends<br />

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