首页> 外文期刊>Land Degradation and Development >ASSESSMENT OF LAND COVER CHANGES AND THEIR EFFECT ON SOIL ORGANIC CARBON AND SOIL TOTAL NITROGEN IN DAQING PREFECTURE, CHINA
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ASSESSMENT OF LAND COVER CHANGES AND THEIR EFFECT ON SOIL ORGANIC CARBON AND SOIL TOTAL NITROGEN IN DAQING PREFECTURE, CHINA

机译:大庆地区土地覆盖变化及其对土壤有机碳和土壤全氮的影响。

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The aim of this study was to examine the influence of land cover changes on soil organic carbon (SOC) and soil total nitrogen (STN) in the Daqing Prefecture of China, where heavy industrialisation in the form of dense oil wells has impacted the environment. Time-series presentations for the period 1978 to 2008 of remotely sensed data and soil survey data were used to assess the extent of the changes. The study revealed soil degradation under all land cover types and in all soil types, grassland retreat (-15 per cent), swampland retreat (-45 per cent) and increases in the area of farmland (+19 per cent), sand land (+1450 per cent) and alkaline land (+52 per cent). Depletion of the SOC pool occurred in swampland (-64 per cent) both because of the decrease in the area of swampland and because of a decrease in SOC density (-34 per cent). An increase in the SOC pool occurred in alkaline land because of the increase in the area and also because of an increase in SOC density (+297 per cent), but there was little change in the SOC pool in farmland because the increase in area was largely offset by a decrease in SOC density (-14 per cent). The decrease in the STN pool was substantial (-44 per cent), with the largest contributor being the decrease in swamplands (-74 per cent), partly because of the decrease in the area of swampland and partly because of a decrease in STN density (-52 per cent). Large decreases in the STN pool also occurred in farmland (-22 per cent) and grassland (-41 per cent). The direct impacts of construction associated with the expansion of the oil industry were overshadowed by indirect impacts such as interference with water flows and water levels resulting in salinisation of soil. The study also revealed that land cover changes are much more dynamic than a simple analysis would reveal, and because of lag times in the loss of SOC, soil degradation will continue even if land cover changes cease. Copyright (c) 2012 John Wiley & Sons, Ltd.
机译:这项研究的目的是研究中国大庆地区土地覆盖变化对土壤有机碳和土壤总氮的影响,那里的重工业化以稠密油井的形式影响了环境。利用1978年至2008年的时间序列表述的遥感数据和土壤调查数据来评估变化的程度。研究表明,在所有土地覆盖类型和所有土壤类型下,草地退缩(-15%),沼泽退缩(-45%),农田面积增加(+ 19%),沙地( + 1450%)和碱性土地(+ 52%)。由于沼泽地面积的减少和SOC密度的减少(-34%),沼泽地的SOC库发生了消耗(-64%)。由于面积的增加以及SOC密度的增加(+ 297%),碱性土地的SOC池增加了,但由于面积的增加,农田的SOC池几乎没有变化。 SOC密度的下降(​​-14%)在很大程度上被抵消了。 STN池大量减少(-44%),最大的贡献是沼泽地减少(-74%),部分原因是沼泽地面积减少,部分是因为STN密度减少(-52%)。在农田(-22%)和草地(-41%)中,STN库也大量减少。与石油工业的扩张有关的建筑的直接影响被诸如水流和水位的干扰导致土壤盐碱化等间接影响所掩盖。该研究还表明,土地覆盖的变化比简单的分析要动态得多,并且由于SOC损失的滞后时间,即使土地覆盖的变化停止,土壤退化也将继续。版权所有(c)2012 John Wiley&Sons,Ltd.

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