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For example, cultivation of land leads to a release of soil C ranging from 30 to 60% of the original stock in the topsoil [5, 6].
The opposing effects were attributed to combined effects of SDS on TCE desorption and degradation, release of soil organic matter and nanoparticle aggregation.
Unplanned road construction without proper drainage tends to accumulate water and channel it in ways that lead to gullying, greater release of soil volumes, roadside failures and shallow landslides, especially in areas with such intense rainfall events, such as Phewa watershed.
By studying the changes in soil retained and soluble P pooloccurring during the growth of two legumes in two scenarios of contrasting P availability we aimed to describe the release of soil retained P, organic and inorganic, into the soluble pools and to relate it to changes in organic C during crop growth.
We therefore expect that chronic increases in litterfall will induce a substantial release of soil carbon in the medium term.
Increased availability of P has been observed in both planted and invasive Pinus (Chen et al. 2008; Dickie et al. 2011), as has a release of soil C (Chapela et al. 2001; Dickie et al. 2011).
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Release of soil-bound iodine has also been observed in two forest soils (9 56-fold increase) under flooded, anaerobic conditions (Yuita, 19 56-fold
Our results suggest that soil internal forces induce soil aggregate breakdown and then release of fine soil particles when the soil was wetted, supplying the original material for splash erosion.
This phenomenon led to soil aggregate breakdown and release of fine soil particles.
The ARC model consists of three components—availability of groundwater resources (A), groundwater release potential of soil matrix (R), and cost for groundwater extraction (C).
GWD is groundwater development; A is availability of groundwater resources; R is groundwater release potential of soil matrix; C is cost for groundwater extraction.
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