首 页 网络介绍 CERN新闻 规章制度 在研项目 论文与出版物 学术动态 生态知识 人员招聘 人员组成 English

    论文与出版物
   SCI论文目录
   SCI论文全文(PDF文件)
   核心期刊论文目录
   出版物目录
   研究报告目录

 核心期刊论文目录
Concentrations and exports of solutes from surface runoff in Houzhai Karst Basin,southwest China
------------------------------------------------------------------------------------------
出 版 社:Chemical Geology  
发表时间:2012  
台  站: 鼎湖山森林生态系统定位研究站  
作  者:闫俊华等  
点 击 率:367231
------------------------------------------------------------------------------------------
关 键 字(英文):Karst,Chemical export,Surface runoff,Dissolved inorganic carbon  
摘  要(英文):Chemical concentrations and export rates from surface water were analyzed in Houzhai Karst Basin (HKB, area 80.65km2 in total), southwest China, for the past two decades from 1986 to 2007. Surface water chemistry was dominated by ions of calcium (Ca2+), magnesium (Mg2+), bicarbonate (HCO3−) and sulfate (SO4 2−),which together made up 96% (by weight) of the total dissolved solids measured in this study. Seasonal variability of chemical export rates was positively correlated with surface runoff discharge, with the concentrations generally diluting at high discharge. From 1986 to 2007, as a result of the responses of karst weathering to climatic factors, the concentrations of Ca2+, Mg2+, HCO3−, and SO42− slowly increased in surface water. By contrast, changes in the concentrations of sodium (Na+), potassium (K+), and chloride (Cl−) showed a slowly decreasing pattern. We also found that the annual dissolved inorganic carbon (DIC) flux ranged from 10.1 to 34.1gCm−2 yr−1, with an average value of 24.2gCm−2 yr−1. Rainfall had the most important influence on DIC flux, although water pH may greatly affect the proportions of the three fractions (CO2,HCO3−, CO3 2−) of DIC. High water temperature in the wet season may reduce the solubility of CO2 in water and consequently affect DIC export rate, but this effect is much smaller than that of rainfall. Based on the chemical mass balance in surface water, our results indicate that high concentrations of SO4 2− by the large gypsum (CaSO4·2H2O) dissolution offset some anions such as HCO3− in karst water, which can partly explain why carbon uptake is often overestimated by the empirical model using concentrations of HCO3− in this karst water. It is concluded that the fluvial flux of DIC from karst water is important to the regional or national carbon budgets.  
------------------------------------------------------------------------------------------
闫俊华-2012-Chemical Geology-Concentrations and exports of solutes from surface runoff in Houzhai Karst Basin,southwest China.pdf
相关文章:
Dynamics of profiles and storage of carbon dioxide in broadleaved/Korean forest in Changbai Mountain
长白山阔叶红松林的零平面位移和粗糙度
长白山阔叶红松林二氧化碳浓度特征
长白山阔叶红松林热量平衡和蒸散的研究
长白山阔叶红松林生长季热量平衡变化特征
长白山阔叶红松林通量观测的footprint及源区分布
长白山阔叶红松林C02交换的涡动通量修订
单株树的阻力系数模式
冠层尺度的生态系统光合-蒸腾耦合模型研究
拉格朗日逆分析在森林蒸散模拟中的应用
相关文章分页:  共 201 页 2006 条记录 9 3[81][82][83][84][85][86][87][88][89][90]4 :

[关闭窗口]
中国生态系统研究网络 版权所有
| 网络介绍 | 联系方式 | 网站地图 |