| 重庆西部山区典型湖泊水-气界面CO2交换通量及其影响因素 |
| 摘要点击 1991 全文点击 707 投稿时间：2018-05-07 修订日期：2018-07-07 |
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| 中文关键词 CO2吸收 山区湖泊 薄边界层法 静态箱法 环境因子 |
| 英文关键词 CO2 absorption mountainous lake thin boundary layer method static chamber method environmental factor |
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| 中文摘要 |
| 为了解我国西南山区湖泊水体CO2的释放/吸收特征，于2017年7月对重庆西部山区典型9个湖泊表层水体溶解性无机碳进行调查，并同步监测关键环境因子，运用薄边界层法和静态箱法对其水-气界面CO2通量[F（CO2）]进行比较研究.结果表明，渝西山区湖泊夏季表层水p（CO2）介于2.1~45.0 Pa之间，均值为（18.1±12.1）Pa；模型法和静态箱法计算的CO2通量均值分别为（-8.0±2.9）、（-3.4±3.6）和（-7.1±22.3）mmol·（m2·d）-1，总体表现出大气CO2汇的特征.水体p（CO2）和F（CO2）与关键环境因子的相关分析，表明表层水p（CO2）和F（CO2）与风速和ORP显著正相关，与pH显著负相关. |
| 英文摘要 |
| To examine the mountainous lake CO2 evasion in Southwest China, partial pressures of carbon dioxide[p(CO2)] and the CO2 exchange flux[F(CO2)] via the water-air interface of nine mountainous lakes in Chongqing, China, have been studied in summer using the thin boundary layer model (TBL) and floating chambers. Key water quality parameters were concomitantly measured. The results indicate that the pCO2 in the mountainous lakes in western Chongqing ranges from 2.1 to 45.0 Pa, with a mean value of (18.1±12.1) Pa. The mean CO2 fluxes calculated by the TBL model and chamber method are (-8.0±2.9), (-3.4±3.6), and (-7.1±22.3) mmol·(m2·d)-1, respectively. The p(CO2) and F(CO2) have positive correlations with the wind speed and ORP but negative correlations with the pH. Our study indicates that mountainous lakes are atmospheric sinks of CO2 and the TBL model should be cautiously adopted. |
