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分析黑河流域关键土地退化和发展过程及其驱动机制。

Analysis of critical land degradation and development processes and their driving mechanism in the Heihe River Basin.

机构信息

School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China.

School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China; Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China.

出版信息

Sci Total Environ. 2020 May 10;716:137082. doi: 10.1016/j.scitotenv.2020.137082. Epub 2020 Feb 3.

Abstract

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.

摘要

在干旱地区,土地开发与退化(LDD)是由不良的土地开发、人类生产和生活以及气候变化所维持的。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障生态环境的可持续发展具有重要意义。本研究通过对关键土地利用动态的时空评价及其土地质量变化趋势,探讨了 1990-2010 年期间黑河流域(HRB)的关键土地退化过程。然后,通过一个同时考虑三个过程相互作用的联立方程模型,分析了耕地开发过程、草地退化过程和水资源变化过程的驱动机制。结果表明,1990 年至 2010 年间,耕地的相互转移主要集中在中游。其面积增长了 13.5%,平均动态度保持在 0.61%。草地和耕地、未利用地之间的转移更为显著,导致草地质量下降,甚至草地退化。水域面积保持动态平衡,面积几乎不变,但动态趋势最初是增加,然后减少。然而,整个研究区土地质量的平均退化程度在持续缓解。这些变化主要是由于上述土地退化过程的相互作用,以及社会经济和气候变化的影响。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,是否为主要粮食产区的变量是该地区草地和水资源退化的主要驱动因素。这些结论将为 HRB 的生态土地恢复和土地质量改善提供科学参考。

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