2013
DOI: 10.1007/s11104-013-1606-3
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Quantitative effects of wind erosion on the soil texture and soil nutrients under different vegetation coverage in a semiarid steppe of northern China

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Cited by 78 publications
(41 citation statements)
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“…Previous studies have reported that soil C and N stocks in the upper soil layers were positively correlated with MAP and negatively correlated with MAT; these findings are similar to our observations along a large aridity gradient (Follett et al, 2012;He et al, 2014;Liu et al, 2012;Miller et al, 2004). The depletion of fine soil particles due to the intensified wind erosion with increasing aridity could further deplete C and nutrients in arid systems because these particles have disproportionately greater amounts of C and nutrients than larger particles (Yan et al, 2013). Furthermore, the decline of plant coverage and aboveground biomass under higher aridity would also contribute to the decreased C and N content along this aridity gradient.…”
Section: Discussionsupporting
confidence: 91%
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“…Previous studies have reported that soil C and N stocks in the upper soil layers were positively correlated with MAP and negatively correlated with MAT; these findings are similar to our observations along a large aridity gradient (Follett et al, 2012;He et al, 2014;Liu et al, 2012;Miller et al, 2004). The depletion of fine soil particles due to the intensified wind erosion with increasing aridity could further deplete C and nutrients in arid systems because these particles have disproportionately greater amounts of C and nutrients than larger particles (Yan et al, 2013). Furthermore, the decline of plant coverage and aboveground biomass under higher aridity would also contribute to the decreased C and N content along this aridity gradient.…”
Section: Discussionsupporting
confidence: 91%
“…Given the predicted increases in aridity in this century for the global drylands (Dai, 2013), this study indicates that the soil C and N pools in those arid ecosystems may decline in the future. Because wind erosion would lead to greater loss of relatively fine silt and clay particles (Yan et al, 2013), our results suggest that land use practices which reduce wind erosion (e.g. reducing the intensity of grazing) will play an important role in sustaining soil C sequestration in dryland regions globally.…”
Section: Discussionmentioning
confidence: 91%
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“…In addition, reclamation might result in a higher percentage of macro-aggregate of coastal reclaimed soils, especially for old zone 1930s that was closer to the residential zone. Previous studies have presented soil quality as possibly being improved by increasing vegetation coverage to prevent soil erosion and decrease the loss of fine particles, especially in the rainy seasons after the crops are harvested [47]. For soil pH, the median value displayed a slightly declining trend from 8.47 to 7.60 with the increase of reclamation time, but the ANOVA showed a significant difference from the intertidal flats to the 1930s soils (p<0.05).…”
Section: Variance Analysis For Soil Properties In Different Zonesmentioning
confidence: 88%
“…The average elevation at the site is 650 m, and the site features a flat surface that does not vary by more than 20 m in elevation. The regional climate is characterized as a semiarid steppe with an annual average rainfall of 350-400 mm, which mainly occurs from July to September [32]. The land cover is meadow steppe, which is dominated by Leymus chinensis and Stipa baicalensis.…”
Section: Site Descriptionmentioning
confidence: 99%