浙江省灵江流域地表水化学特征及灌溉适宜性
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P641.3

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中国地质调查局项目“浙南诸河流域地下水资源调查评价”(DD20211572,ZD20220215,DD20230507)


Chemical Characteristics of Surface Water and Suitability for Irrigation at Lingjiang River Basin in Southern Zhejiang Province
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    摘要:

    [目的] 灵江是浙南诸河流域重要河流,在浙南一带具有典型性和代表性。分析灵江流域地表水体的水化学特征和演化机理及其灌溉适宜性,为该区域生态保护和高质量发展提供科学依据。[方法] 综合利用数理统计、Piper三线图、主成分分析和离子比等方法对流域地表水体进行水化学统计分析及成因判别;通过绘制Wilcox图和USSL图评估流域内地表水体灌溉适宜性。[结果] ① 灵江流域地表水的化学类型在空间上具有分带性。从中上游(Ⅰ区)-下游温黄平原河网区(Ⅱ区)-台州湾入海口(Ⅲ区)水化学类型从HCO3-Ca型向Cl-Na型过渡。②Ⅰ区地表水的化学特征主要受到岩石风化作用中的硅酸盐岩溶解影响,少量受碳酸盐岩溶解影响;Ⅱ区地表水的水化学特征主要受硅酸盐岩溶解影响,Ⅲ区地表水的化学特征主要受蒸发盐岩溶解影响。③Ⅰ,Ⅱ区地表水的K+,Na+主要来源于硅酸盐矿物溶解,Ca2+,Mg2+,HCO-3,SO2-4主要受硅酸盐岩溶解,少量来源于碳酸盐岩的溶解。NO-3则主要来源于人类活动。④Ⅰ,Ⅱ区地表水适用于农业灌溉,Ⅲ区地表水灌溉适宜性较差,易引起盐碱害。[结论] 灵江流域地表水体的水化学组分受天然溶解及人类活动共同影响,中上游和下游温黄平原河网区地表水适宜农业灌溉,台州湾入海口地表水易引起盐碱害,在制定农业灌溉及生态保护和高质量发展规划时应予以重视。

    Abstract:

    [Objective] Lingjiang River is an important river basin in Southern Zhejiang Province, which is typical and representative. The hydrochemical characteristics, evolutionary mechanism and irrigation suitability of surface water at Lingjiang River basin were analyzed in order to provide scientific basis for agricultural irrigation, ecological protection and high-quality development in this region.[Methods] Mathematical statistics, Piper three-line graphs, principal component analysis, and ion ratio were used to analyze the hydrochemical statistics and identify the causes of the surface water in the basin. The suitability of surface water for irrigation was evaluated by constructing Wilcox diagrams and USSL diagrams.[Results] ① The hydrochemical types of surface water at Lingjiang River basin were spatially zoned, and the hydrochemical types from HCO3-Ca type to Cl-Na type transitioned from the middle and upper reaches (zone Ⅰ) to the lower reaches of the Wenhuang Plain (zone Ⅱ) to the estuary of Taizhou Bay (zone Ⅲ). ② The hydrochemical characteristics of the surface water in zone Ⅰ were mainly affected by the dissolution of silicate rock during rock weathering, and were affected to a lesser extent by the dissolution of carbonate karst. The hydrochemical characteristics of surface water in zone Ⅱ were mainly affected by the dissolution of silicate rock. The hydrochemical characteristics of surface water in zone Ⅲ were mainly affected by the dissolution of evaporative salt rocks. ③ The K+ and Na+ of the surface water in zones Ⅰ and Ⅱ were mainly from the dissolution of silicate minerals. Ca2+, Mg2+, HCO-3, and SO2-4 mainly resulted from the dissolution of silicate rock, and a small amount resulted from the dissolution of carbonate rock, NO-3 was mainly derived from human activities. ④ The surface water in zones Ⅰ and Ⅱ was suitable for agricultural irrigation, while the surface water in zone Ⅲ was poorly suited for irrigation, and could easily cause saline-alkali damage.[Conclusion] The hydrochemical components of surface water at Lingjiang River basin were affected by natural dissolution and human activities. The surface water in the river network area of the middle and upper reaches and lower reaches of the Wenhuang Plain is suitable for agricultural irrigation, while the surface water in the estuary of Taizhou Bay is prone to saline-alkali damage. Attention should be paid to the planning of agricultural irrigation and ecological protection and high-quality development.

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周施阳,向翻,袁东方,姚飞延,董好刚,吴鑫,王震威,李振.浙江省灵江流域地表水化学特征及灌溉适宜性[J].水土保持通报,2024,44(1):57-67

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  • 收稿日期:2023-07-22
  • 最后修改日期:2023-08-30
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  • 在线发布日期: 2024-04-26
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