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OALib Journal期刊
ISSN: 2333-9721
费用：99美元
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藏南羊卓雍错流域水化学区域差异及其成因
DOI: 10.11821/xb201301006, PP. 36-44
Keywords: 水化学性质,地质,水文条件,羊卓雍错流域
Abstract:
特殊的地理环境造成青藏高原高寒区水化学性质及其动态的特殊性。本文通过对藏南羊卓雍错流域进行水样采集、分析与测定,探讨了该流域水化学性质的区域差异及其成因。结果表明,羊卓雍错流域水化学性质区域差异明显主要是自然因素综合作用的结果,而人类活动对区域水化学性质亦有所贡献。首先,在特殊的高寒气候条件下,流域内各湖泊水化学性质差异的根本原因是其水文条件不同。其次,羊卓雍错西南部湖水样品中硼和锂含量偏高说明该区域湖相沉积中可能存在硼酸盐矿物和含锂菱镁矿。第三,流域东部和西部河水化学性质差异明显的主因是河流所经地区地质条件不同;羊卓雍错南岸和北岸地下水化学性质差异的关键则是区域水系发育程度不同。此外,巴纠错、嘎马林河和羊卓雍错南岸水井样品的总氮含量较高,这反映了人类活动对区域水化学性质的影响。
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