| 湿地土壤气体排放对水位变化响应的持续性动态特征 |
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| 引用本文： | 吕海波.湿地土壤气体排放对水位变化响应的持续性动态特征[J].干旱区地理,2022,45(3):860-866. |
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| 作者姓名： | 吕海波 |
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| 作者单位： | 1.渭南师范学院环境与生命科学学院,陕西 渭南 7140002.陕西省河流湿地生态与环境重点实验室,陕西 渭南 714000 |
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| 基金项目： | 陕西省教育厅创新团队项目 |
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| 摘 要： | 为探索湿地水位变化与土壤气体排放之间的关系,对黄河中游芦苇湿地进行了半注水和满注水样地处理后的动态监测,对比了7 d水位变化过程中土壤气体排放差异。结果表明：注水造成了土壤CO2排放速率的显著差异;随土壤温度上升,H2O、CO2、H2S排放速率都有上升趋势（满注水样地的H2O除外）;半注水和满注水造成的影响,H2O排放速率表现为趋同-异步-消失的特征,在注水前期（63.73 h）半注水和满注水差异基本一致,后期差异较大,直至125.64 h后注水的影响才消失,总体分别造成H2O排放总量76.3%和31.3%的增加;CO2排放速率表现为异步-趋同的特征,注水初期环境的改变造成CO2排放的一致减少,37.69~68.66 h二者出现明显差异,68.66~125.64 h水位虽然恢复,但差异仍然存在,注水分别造成CO2排放总量50.1%和43.2%的减少;H2S排放速率表现为无变化-异步-无变化的特征,总体造成H2S排放总量42.3%和32.3%的增加。研究追踪了水位上升后土壤H2O、CO2和H2S排放速率变化的动态过程,其影响具有异步性和持续性的特点,CO2排放速率表现出较长的响应周期。研究结果对于河流湿地生态功能研究具有重要意义,湿地土壤气体排放对水位变化的响应滞后意味着对湿地生态功能的重要影响,其波动过程需要更长时段的精准研究。
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| 关 键 词： | 土壤CO2排放 湿地水位变化 生态功能 注水试验 |
| 收稿时间： | 2021-07-13 |
Continuous dynamic characteristics of wetland soil gas emission response to water level changes |
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| LYU Haibo.Continuous dynamic characteristics of wetland soil gas emission response to water level changes[J].Arid Land Geography,2022,45(3):860-866. |
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| Authors: | LYU Haibo |
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| Affiliation: | 1. College of Environmente and Life Sciences, Weinan Normal University, Weinan 714000, Shaanxi, China2. Key Laboratory of River Wetland Ecology and Environment in Shaanxi Province, Weinan 714000, Shaanxi, China |
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| Abstract: | Wetlands have an ecological purpose that is correlated with global climate change. On the background of climate change, the spatial and temporal variations of global precipitation amplify the effect on the water environment of river wetlands via catchment confluence, affecting the ecological function of wetlands significantly. To examine the relationship between wetland water level changes and soil gas emission, half water injection and full water injection treatments were considered in reed wetlands in the middle reaches of the Yellow River in China, and the differences in soil gas emission during the 7-day monitored were compared. Compared with natural sites, water injection created a significant difference in soil CO2 emission rate. Except for the H2O emission rate of full water injection, H2O, CO2, and H2S emission rates all considered upward trend with soil temperature rising. In the monitoring process, for the effect of half and full water injection, H2O emissions rate half and full water injection were basically the same, while the difference was higher in the later stage, the effect of did not disappear until 125.64 h, totally water injection resulted in an increase of 76.3% and 31.3% respectively; CO2 emissions rate appeared asynchronous-converging characteristics, the changes of environment in the initial stage resulted in the consistent reduction of CO2 emission, and considered a significant difference between 37.69 h and 68.66 h, although the water level recovered from 68.66 h to 125.64 h, the differences still existed, water injection resulted in a reduction of CO2 total emissions by 50.1% and 43.2% respectively. H2S emissions rate experienced changeless-asynchronous-changeless process, and totally, resulted in 42.3% and 32.3% increase. The study tracked the dynamic process of soil H2O, CO2, and H2S emission rates after water level rise and found that the effect of a rise of water level on the soil gas emission rate was asynchronous and persistent, demonstrating a long response cycle to CO2 emissions rate. The results consider high significance to the ecological function of river wetlands, the delayed response of wetland soil gas emission to water level change means that it has a significant effect on wetland ecological function, its fluctuation process needs a longer period of accurate study. |
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| Keywords: | soil CO2 emission changes of wetland water level ecological function the water injection test |
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