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Modelling of sand/dust emission in Northern China from 2001 to 2014

机译:2001至2014年中国北方沙子/尘埃发射的建模

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Wind erosion is a major contributing factor to soil degradation and environmental pollution. As a hot spot of wind erosion, Northern China suffers from severe wind erosion hazards. Besides, there is an ongoing controversy regarding the magnitudes of sand/dust emissions of anthropogenic sources. To understand the mechanism of soil degradation and environmental pollution caused by wind erosion, and to resolve the controversy whether sand/dust emissions is from natural or anthropogenic sources in Northern China, accurate spatio-temporal distributions of sand/dust emission should be obtained. Herein, a wind erosion model with a high spatio-temporal resolution was developed and employed to identify the sand and dust emissions of areas with different land cover types. The sand and dust emission hot spots from 2001 to 2014 were mainly distributed in the Gashun Gobi and Kumutage Deserts, those are all natural areas. In these regions, the average sand and dust emissions exceeded 10,000 kg/m/y (year) and 240 g/m(2)/y, respectively. The intensities of sand and dust emissions demonstrated significant decreasing trends during this time. According to Moderate Resolution Imaging Spectroradiometer (MODIS) land cover data, the average sand/dust emission rates in natural sources were much higher than that in anthropogenic areas, e.g. from 2001 to 2014, the average annual dust emission of Northern China was about 130 Tg/y, and only approximately 3.7% of dust emissions originated from anthropogenic areas. Dust deflation correspondingly caused the entrainment of soil nutrients into atmosphere and result in soil degradation. Our results also show that the Soil Organic Carbon (SOC) loss due to wind erosion in Northern China was about 0.9 Tg/y and that 32.5% and 7.5% of the SOC loss originated from grasslands (including woody savannas, savannas, and grasslands) and farmlands (including croplands and cropland/natural vegetation mosaics), respectively. With regard to such severe sand and dust emissions, we believe that the results of this study could provide valuable information for the creation of strategies to cope with wind erosion hazards and measures to control the extent of wind-blown sand. In addition, the proposed model could be of interest to ecological and environmental researchers.
机译:风侵蚀是土壤退化和环境污染的主要贡献因素。作为风侵蚀的热点,中国北方遭受了严重的风蚀危害。此外,关于人为源的砂/粉尘排放量大持续争议。要了解风侵蚀造成的土壤退化和环境污染的机制,并解决砂/粉尘排放是从中国北方的天然或人为来源的争议,应得到准确的砂/粉尘排放的时空分布。这里,开发出具有高时空分辨率的风蚀模型,并采用具有不同陆地覆盖类型的区域的砂和灰尘排放。 2001年至2014年的沙子和灰尘排放热点主要分布在Gashun Gobi和Kumutage沙漠中,这些都是自然地区。在这些区域中,平均砂和粉尘排放量分别超过10,000kg / m / y(年)和240g / m(2)/ y。沙子和粉尘排放的强度在此期间显着降低了趋势。根据中等分辨率的成像分光镜(MODIS)覆盖数据,天然来源的平均砂/粉尘排放率远高于人为区域,例如在人为区域中。从2001年到2014年,中国北方的平均尘埃排放约为130 TG / Y,只有大约3.7%的粉尘排放来自人为地区。灰尘通缩相应地导致土壤养分夹带到大气中并导致土壤降解。我们的研究结果还表明,中国北部风腐蚀的土壤有机碳(SOC)损失约为0.9 TG / Y,32.5%和7.5%的SoC丧失来自草地(包括木本大草原,大草原和草原)和农田(包括农田和农田/天然植被马赛克)。关于这种严重的沙子和灰尘排放,我们认为这项研究的结果可以提供有价值的信息,以创造应对风险侵蚀危害和控制风吹沙子程度的策略。此外,拟议的模型可能对生态和环境研究人员感兴趣。

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