Knowledge Resource Center for Ecological Environment in Arid Area
Soil respiration in typical plant communities in the wetland surrounding the high-salinity Ebinur Lake | |
Li Yanhong; Zhao Mingliang; Li Fadong | |
来源期刊 | Frontiers of Earth Science
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ISSN | 2095-0195 |
出版年 | 2018 |
卷号 | 12期号:3页码:611-624 |
英文摘要 | Soil respiration in wetlands surrounding lakes is a vital component of the soil carbon cycle in arid regions. However, information remains limited on the soil respiration around highly saline lakes during the plant growing season. Here, we aimed to evaluate diurnal and seasonal variation in soil respiration to elucidate the controlling factors in the wetland of Ebinur Lake, Xinjiang Uygur Autonomous Region, western China. We used a soil carbon flux automatic analyzer (LI-840A) to measure soil respiration rates during the growing season (April to November) in two fields covered by reeds and tamarisk and one field with no vegetation (bare soil) from 2015 to 2016. The results showed a single peak in the diurnal pattern of soil respiration from 11:00 to 17:00 for plots covered in reeds, tamarisk, and bare soil, with minimum values being detected from 03:00 to 07:00. During the growing season, the soil respiration of reeds and tamarisk peaked during the thriving period (4.16 and 3.75 mmol·m~(-2)·s~(-1), respectively), while that of bare soil peaked during the intermediate growth period (0.74 mmol·m~(-2)·s~(-1)). The soil respiration in all three plots was lowest during the wintering period (0.08, 0.09, and - 0.87 mmol·m~(-2)·s~(-1), respectively). Air temperature and relative humidity significantly influenced soil respiration. A significant linear relationship was detected between soil respiration and soil temperature for reeds, tamarisk, and bare soil. The average Q_(10) of reeds and tamarisk were larger than that of bare soil. However, soil moisture content was not the main factor controlling soil respiration. Soil respiration was negatively correlated with soil pH and soil salinity in all three plot types. In contrast, soil respiration was positively correlated with organic carbon. Overall, CO_2 emissions and greenhouse gases had a relatively weak effect on the wetlands surrounding the highly saline Ebinur Lake. |
英文关键词 | Ebinur Lake soil respiration high salinity soil temperature soil moisture |
类型 | Article |
语种 | 英语 |
收录类别 | CSCD |
WOS研究方向 | Science & Technology - Other Topics |
CSCD记录号 | CSCD:6326501 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/335998 |
作者单位 | Li Yanhong, Xinjiang Normal University, College of Geography and Tourism;;Key Laboratory of Xinjiang Uygur Autonomous Region;;Xinjiang Laboratory of Lake Environment and Resources in Arid Area, ;;Key Laboratory of Xinjiang Uygur Autonomous Region;;Xinjiang Laboratory of Lake Environment and Resources in Arid Area, Urumqi;;Urumqi, ;; 830054;;830054.; Zhao Mingliang, Xinjiang Normal University, College of Geography and Tourism;;Key Laboratory of Xinjiang Uygur Autonomous Region;;Xinjiang Laboratory of Lake Environment and Resources in Arid Area, ;;Key Laboratory of Xinjiang Uygur Autonomous Region;;Xinjiang Laboratory of Lake Environment and Resources in Arid Area, Urumqi;;Urumqi, ;; 830054;;830054.; Li Fadong, Xinjiang Normal University, College of Geography and Tourism;;Key Laboratory of Xinjiang Uygur Autonomous Region;;Xinjiang Laboratory of Lake Environment and Resources in Arid Area;;Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences;;College of Resources an... |
推荐引用方式 GB/T 7714 | Li Yanhong,Zhao Mingliang,Li Fadong. Soil respiration in typical plant communities in the wetland surrounding the high-salinity Ebinur Lake[J],2018,12(3):611-624. |
APA | Li Yanhong,Zhao Mingliang,&Li Fadong.(2018).Soil respiration in typical plant communities in the wetland surrounding the high-salinity Ebinur Lake.Frontiers of Earth Science,12(3),611-624. |
MLA | Li Yanhong,et al."Soil respiration in typical plant communities in the wetland surrounding the high-salinity Ebinur Lake".Frontiers of Earth Science 12.3(2018):611-624. |
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