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World’s Soil Resources

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Figure 6.2 Location of active and fixed aeolian deposits. Source: Thomas and Wiggs, 2008.<br />

6.1.3 | <strong>Soil</strong> erosion versus soil formation<br />

The accelerated loss of topsoil through erosion from agricultural land was recognized as an important<br />

threat to the world’s soil resource many decades ago. Furthermore, it was feared that soil was, in many areas,<br />

eroding much faster than that it could be replaced through soil formation processes. More recent studies have<br />

confirmed that these early observations were not just perceptions. Estimated rates of soil erosion of arable or<br />

intensively grazed lands have been found to be 100 -1 000 times higher than natural background erosion rates.<br />

These erosion rates are also much higher than known soil formation rates which are typically well below 1<br />

tonnes ha -1 yr -1 with median values of ca. 0.15 tonnes ha -1 yr -1 . The large difference between erosion rates under<br />

conventional agriculture and soil formation rates implies that we are essentially mining the soil and that we<br />

should consider the resource as non-renewable.<br />

The imbalance between erosion rates under conventional agriculture and the rate of soil formation implies<br />

that conventional agriculture on hilly land is not sustainable because the soil resource is mined and will<br />

ultimately become depleted. This has most likely already happened in many areas around the Mediterranean<br />

Sea and in tropical mountain regions. So-called soil loss tolerance levels may help to set objectives for shortterm<br />

action. However, long-term sustainability requires that soil erosion rates on agricultural land are reduced<br />

to near-zero levels.<br />

Figure 6.3 <strong>Soil</strong> relict in the Jadan basin, Ecuador.<br />

Photo by G. Govers<br />

In this area overgrazing led to excessive erosion and the soil<br />

has been completely stripped from most of the landscape<br />

in less than 200 years, exposing the highly weathered<br />

bedrock below. The person is standing on a small patch of<br />

the B-horizon of the original soil that has been preserved.<br />

Picture credit: Gerard Govers.<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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