Hu Xiaoli, Lu Ling, Li Xin, Wang Jianhua, Guo Ming
Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, 320 Donggang West Road, Lanzhou, 730000, China.
PLoS One. 2015 Jun 26;10(6):e0128960. doi: 10.1371/journal.pone.0128960. eCollection 2015.
The Heihe River Basin (HRB) is a typical arid inland river basin in northwestern China. From the 1960s to the 1990s, the downstream flow in the HRB declined as a result of large, artificial changes in the distribution of water and land and a lack of effective water resource management. Consequently, the ecosystems of the lower reaches of the basin substantially deteriorated. To restore these degraded ecosystems, the Ecological Water Diversion Project (EWDP) was initiated by the Chinese government in 2000. The project led to agricultural and ecological changes in the middle reaches of the basin. In this study, we present three datasets of land use/cover in the middle reaches of the HRB derived from Landsat TM/ETM+ images in 2000, 2007 and 2011. We used these data to investigate changes in land use/cover between 2000 and 2011 and the implications for sustainable water resource management. The results show that the most significant land use/cover change in the middle reaches of the HRB was the continuous expansion of farmland for economic interests. From 2000 to 2011, the farmland area increased by 12.01%. The farmland expansion increased the water resource stress; thus, groundwater was over-extracted and the ecosystem was degraded in particular areas. Both consequences are negative and potentially threaten the sustainability of the middle reaches of the HRB and the entire river basin. Local governments should therefore improve the management of water resources, particularly groundwater management, and should strictly control farmland reclamation. Then, water resources could be ecologically and socioeconomically sustained, and the balance between upstream and downstream water demands could be ensured. The results of this study can also serve as a reference for the sustainable management of water resources in other arid inland river basins.
黑河流域是中国西北典型的干旱内陆河流域。从20世纪60年代到90年代,由于水土分布的大规模人为变化以及缺乏有效的水资源管理,黑河流域下游径流量减少。因此,流域下游的生态系统严重退化。为恢复这些退化的生态系统,中国政府于2000年启动了生态输水工程。该工程导致了流域中游的农业和生态变化。在本研究中,我们展示了源自2000年、2007年和2011年陆地卫星TM/ETM+影像的黑河流域中游土地利用/覆盖的三个数据集。我们利用这些数据调查了2000年至2011年期间土地利用/覆盖的变化及其对水资源可持续管理的影响。结果表明,黑河流域中游最显著的土地利用/覆盖变化是出于经济利益的农田持续扩张。2000年至2011年,农田面积增加了12.01%。农田扩张加剧了水资源压力;因此,地下水被过度开采,特定区域的生态系统退化。这两种后果都是负面的,可能威胁到黑河流域中游及整个流域的可持续性。因此,地方政府应加强水资源管理,尤其是地下水管理,并应严格控制农田开垦。这样,水资源才能在生态和社会经济方面得以维持,并确保上下游用水需求的平衡。本研究结果也可为其他干旱内陆河流域的水资源可持续管理提供参考。