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首页> 外文期刊>The Science of the Total Environment >Analysis of critical land degradation and development processes and their driving mechanism in the Heihe River Basin
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Analysis of critical land degradation and development processes and their driving mechanism in the Heihe River Basin

机译:黑河流域关键土地退化与发展过程及其驱动机制分析。

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In arid regions, land development and degradation (LDD) is sustained by the undesirable land development, human production and living, and climate change. Therefore, the understanding of LDD processes and their driving mechanism in the arid or semi-arid regions is significant to guarantee the sustainable development of ecological environment. This study explored the critical LDD processes in the Heihe River Basin (HRB) during 1990-2010 with the spatio-temporal evaluation of critical land use dynamics and its land quality changing trends. Then, the driving mechanism of cultivated land development process, grassland degradation process and water resource change process were analyzed by a simultaneous equations model which took the interaction of three processes into account The results showed that the mutual transfers of cultivated land were primarily gathered in the middle reaches from 1990 to 2010. Its area grew by 13.5% and the average dynamic degree remained at 0.61%. The transfers between grassland and cultivated land, unused land were more remarkable, which led to the decline of grassland quality and even grassland degradation. Water area maintained a dynamic balance with almost unchanged area, but its dynamic trend was initially increasing and then decreasing. However, the average degradation of land quality in the whole study area is continuously alleviated. These changes were mainly due to the interaction of the LDD processes above, as well as socio-economic and climate change. Among them, agricultural research investments could restrain the unordered expansion of cultivated land resource for a relatively short period of time. Meanwhile, the variable of whether it is the main grain producing county is the main driver of grassland and water resource degradation in this region. These conclusions will provide scientific references for ecological land restoration and land quality improvement in the HRB.
机译:在干旱地区,土地开发和退化(LDD)由不良的土地开发,人类生产和生活以及气候变化所支撑。因此,了解干旱或半干旱地区的LDD过程及其驱动机制对于保证生态环境的可持续发展具有重要意义。这项研究探索了1990-2010年黑河流域(HRB)的关键LDD过程,并对关键土地利用动态及其土地质量变化趋势进行时空评估。然后,利用联立方程模型分析了耕地发展过程,草地退化过程和水资源变化过程的驱动机制,该模型考虑了三个过程的相互作用。结果表明,耕地的相互转移主要集中在耕作过程中。 1990年至2010年是中游地区。其面积增长了13.5%,平均动态度保持在0.61%。草地与耕地,未利用土地之间的转移更为显着,导致草地质量下降甚至草地退化。水域保持动态平衡,面积几乎保持不变,但其动态趋势先增大后减小。但是,整个研究区的土地质量平均下降正在不断缓解。这些变化主要归因于上述LDD过程的相互作用,以及社会经济和气候变化。其中,农业研究投资可以在相对较短的时间内抑制耕地资源的无序扩张。同时,是否是粮食主产县的变量是该地区草地和水资源退化的主要驱动力。这些结论将为高铁市的生态土地恢复和土地质量改善提供科学参考。

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