首页|近50年雅鲁藏布江流域上游化学风化及CO2消耗分析

近50年雅鲁藏布江流域上游化学风化及CO2消耗分析

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基于 2013 年、2015 年和 2019-2021 年雅鲁藏布江流域上游连续监测数据,并结合现有研究成果,探究了雅鲁藏布江流域上游近 50 年水化学时空特征演变以及风化速率与 CO2 消耗的变化过程.结果显示,近 50年雅鲁藏布江流域上游河水一直为弱碱性,pH为 7.59~8.54,TDS含量变化呈现出增大的趋势;从 20 世纪70 年代到 21 世纪,硅酸盐岩风化速率变化呈现逐渐增大的趋势,碳酸盐岩风化速率变化呈现出先升后降的变化趋势;流域丰水年硅酸盐岩风化和碳酸盐岩风化消耗的 CO2 通量为 16.90×1010 mol/年,平水年的为10.53×1010 mol/年,枯水年的为 5.74×1010 mol/年,分别占全球大陆硅酸盐岩风化和碳酸盐岩风化消耗CO2通量的 0.80%、0.50%和 0.27%.
Studies on the Chemical Weathering and CO2 Consumption in the Upper Reaches of the Yarlung Tsangpo River in Recent 50 Years
Based on the continuous monitoring data of the upper reaches of the Yarlung Tsangpo River Basin in 2013,2015 and 2019-2021,and combined with the existing research results,the evolution of hydrochemical spatial and temporal char-acteristics and the change process of weathering rate and CO2 consumption in the Yarlung Tsangpo River Basin in recent 50 years were explored.The results show that in recent 50 years,the river water in the Yarlung Tsangpo River Basin has been weakly alkaline,the pH value is between 7.59 and 8.54,and the content change of TDS shows an increasing trend;from the 1970s to the beginning of the 21st century,the weathering rate of silicate rocks showed a gradually increasing trend,and the weathering rate of carbonate rocks showed a changing trend of first increasing and then decreasing;the CO2 flux consumed by silicate rock weathering and carbonate rock weathering is 16.90×1010 mol per year in wet years,is 10.53×1010 mol per year in normal water years,is 5.74×1010 mol per year in dry years,and accounting for 0.80%,0.50%and 0.27%of CO2 flux consumed by global continental silicate rock weathering and carbonate rock weathering respectively.

the Yarlung Tsangpo Riverchemical weatheringCO2 consumptionwater chemistry characteristics

杨剑、汪磊、杨雨超、赵泽阳、韩宇平

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华北水利水电大学 水资源学院,河南 郑州 450046

河南省黄河流域水资源节约集约利用重点实验室,河南 郑州 450046

雅鲁藏布江 化学风化 CO2消耗 水化学特征

国家自然科学基金

41807161

2024

华北水利水电大学学报(自然科学版)
华北水利水电大学

华北水利水电大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.558
ISSN:1002-5634
年,卷(期):2024.45(3)
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