地理学报 ›› 2013, Vol. 68 ›› Issue (1): 36-44.doi: 10.11821/xb201301006
孙瑞1,2, 张雪芹1, 郑度1
收稿日期:
2012-05-10
修回日期:
2012-10-12
出版日期:
2013-01-20
发布日期:
2013-01-20
作者简介:
孙瑞(1985-),女,博士研究生,中国地理学会会员(S110008825M),主要从事青藏高原湖泊研究。E-mail:feifeiry@tom.com
基金资助:
国家自然科学基金项目(41171062; 40871044)
SUN Rui1,2, ZHANG Xueqin1, ZHENG Du1
Received:
2012-05-10
Revised:
2012-10-12
Online:
2013-01-20
Published:
2013-01-20
Supported by:
National Natural Science Foundation of China, No.41171062; No.40871044
摘要: 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。
孙瑞, 张雪芹, 郑度. 藏南羊卓雍错流域水化学区域差异及其成因[J]. 地理学报, 2013, 68(1): 36-44.
SUN Rui, ZHANG Xueqin, ZHENG Du. Spatial variation and its causes of water chemical property in Yamzhog Yumco Basin, South Tibet[J]. Acta Geographica Sinica, 2013, 68(1): 36-44.
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