晋西蔡家川小流域植被恢复区水化学特征

Influence of Long-term Vegetation Restoration on Water Quality in Caijiachuan Small Watershed in Western Shanxi Province

  • 摘要: 研究了自退耕还林以来, 黄土高原地区植被恢复对小流域水质的影响, 为流域水环境质量评价、水资源管理利用及生态环境建设与保护提供参考依据。以晋西黄土丘陵沟壑区蔡家川小流域为研究对象, 依照中国生态系统研究网络森林水环境监测规范, 对小流域地表水和地下水水质开展长期定位监测。采用方差分析检验2006与2023年地表水和地下水水质指标的差异显著性, 采用配对t检验分析汛期与非汛期水质指标的差异。结果表明: (1)2006和2023年蔡家川小流域地表水水体中阴离子以HCO3-浓度为最高, 分别为339.71和384.11 mg·L-1, 地下水水体中阴离子以HCO3-和SO42-浓度为较高, 2006年分别为295.1和120.6 mg·L-1, 2023年分别为351.22和343.89 mg·L-1; 2006年地表水、地下水阳离子均以Ca2+浓度为最高, 分别为46.47和92.2 mg·L-1, 2023年地下水阳离子仍以Ca2+浓度为最高, 为82.97 mg·L-1, 地表水阳离子以Na+浓度为最高, 为56.11 mg·L-1。(2)相较于2006年, 2023年地表水Mg2+和Cl-浓度分别增加74.63%和97.78%, K+浓度减少73.50%, 地下水Mg2+、Na+、SO42-和NO3-浓度分别增加228.77%、44.62%、185.15%和353.64%, K+浓度减少26.67%。(3)2006年, 非汛期地表水TDS、HCO3-浓度和地下水SO42-浓度、pH值显著高于汛期(P < 0.05);2023年, 非汛期地表水COD和地下水Ca2+浓度显著高于汛期(P < 0.05)。植被恢复对于晋西蔡家川小流域地表水和地下水水质有一定改善作用, 但后期人为活动对流域水环境造成了一定污染。研究结果可为小流域水环境综合治理提供科学依据。

     

    Abstract: This study examined the impact of vegetation restoration on water quality in small watersheds of the Loess Plateau since the implementation of the "Grain for Green" policy. The aim was to provide a reference for evaluating watershed water environment quality, optimizing water resource management, and guiding ecological construction and protection efforts. Using the Caijiachuan sub-watershed in the loess hilly and gully region of western Shanxi as the study area, long-term monitoring of surface water and groundwater quality was conducted in accordance with the China Ecosystem Research Network protocols for forest water environment monitoring. Analysis of variance (ANOVA) was employed to test for significant differences in water quality indicators between 2006 and 2023, while paired t-tests assessed seasonal variations between the flood and non-flood seasons. The results reveal the following: (1) The dominant anion in surface water in both 2006 and 2023 was HCO3-, with concentrations of 339.71 and 384.11 mg·L-1, respectively. In groundwater, the dominant anions were HCO3- and SO42-, with concentrations of 295.1 and 120.6 mg·L-1 in 2006, and 351.22 and 343.89 mg·L-1 in 2023, respectively. The dominant cation in both water types in 2006 was Ca2+, at 46.47 mg·L-1 in surface water and 92.2 mg·L-1 in groundwater. In 2023, Ca2+ remained the dominant cation in groundwater (82.97 mg·L-1), while Na+ became dominant in surface water (56.11 mg·L-1). (2) Between 2006 and 2023, Mg2+ and Cl- concentrations in surface water increased by 74.63% and 97.78%, respectively, while K+ decreased by 73.50%. In groundwater, concentrations of Mg2+, Na+, SO42-, and NO3- increased by 228.77%, 44.62%, 185.15%, and 353.64%, respectively, whereas K+ decreased by 26.67%. (3) In 2006, surface water TDS and HCO3- concentrations, along with groundwater SO42- concentration and pH, were significantly higher in the non-flood season than in the flood season (P < 0.05). In 2023, surface water COD and groundwater Ca2+ concentrations were significantly elevated during the non-flood season (P < 0.05). Overall, vegetation restoration improved the water quality of both surface water and groundwater in the Caijiachuan sub-watershed. However, subsequent anthropogenic activities have introduced certain pollutants, indicating the need for continued environmental management. These findings provide a scientific basis for the integrated management of water environment in watershed.

     

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