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首页> 外文期刊>Soil & Tillage Research >In mitigating CO2 emission in the reservoir riparian: The influences of land use and the dam-triggered flooding on soil respiration
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In mitigating CO2 emission in the reservoir riparian: The influences of land use and the dam-triggered flooding on soil respiration

机译:缓解水库河岸中的二氧化碳排放:土地利用对土壤呼吸的影响

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摘要

Soil respiration (SR) has been found to be highly influenced by land use and soil water regimes. However, the relative contribution of farming and dam-triggered flooding in influencing the SR of the riparian zone is poorly understood. The objectives of this study were to investigate the effects of land use and dam-triggered flooding intensity on SR in the riparian zone along the Three Gorges Reservoir (TGR), China, and to identify the main factors shaping the SR. At the Wuyang Bay of the Pengxi River, a tributary of the Yangtze River in the TGR, a series of SR field examinations in different land-use types and along elevation gradients in the riparian zone were carried out from March to September in 2018. During the study period, by analyzing SR in 177 m (elevation above sea level, the same as follows) unflooded site (tJF), 173 m corn field (173C), 173 m paddy field (173 P), 168 m corn field (168C), 168 m paddy field (168 P), 168 m fallow grassland (168 F), 166 m fallow grassland (166 F), 163 m corn field (163C) and 163 m fallow grassland (163 F), significant differences in diurnal variations were found to be mainly affected by soil temperature (ST) at 10 cm depth, while seasonal variations were mainly regulated by ST and rainfall events (i.e. 10 cm depth soil water content). Importantly, croplands were found to contain higher soil organic carbon (SOC) but lower SR efflux and Q(10) values than those for non-cropping fields. The results imply that SR was strongly affected by land-use types rather than flooding intensity in the TGR riparian zone. Furthermore, this study highlights the significant impacts of tillage in stabilizing SOC and reducing SR efflux in the area that is highly influenced by hydrological regime shift. Finally, from the perspective of controlling the soil carbon dioxide emission, we suggest that local government should manage and guide farming activities in the riparian zone.
机译:已发现土壤呼吸(SR)受土地利用和土壤水域的影响很大。然而,农业和大坝触发洪水影响影响河岸区的洪水的相对贡献很差。本研究的目的是调查土地利用和大坝引发洪水强度对沿着三峡库区(TGR),中国的河岸区SR的影响,并确定塑造SR的主要因素。在彭溪河翁溪湾的TGR中长江支流中,在2018年3月至9月,在不同的土地利用类型和沿着河岸地区的海拔梯度中进行了一系列SR田间考试。该研究期,通过分析177米(海拔高度,如下升高),未结合的位点(TJF),173米玉米场(173℃),173米稻田(173p),168米玉米场(168℃ ),168米稻田(168 p),168米休耕草原(168 f),166米休耕草原(166 f),163米玉米田(163c)和163米休耕草原(163°F),昼夜大的差异发现变化主要受到10厘米深度的土壤温度(ST)的影响,而ST和降雨事件(即10cm深水含量)主要调节季节性变化。重要的是,发现农田含有较高的土壤有机碳(SOC),而是低于SR Efflux和Q(10)的值,而不是非裁剪领域。结果意味着SR受土地利用类型而不是TGR河南亚地区的洪水强度受到强烈影响。此外,该研究突出了耕作在稳定SoC稳定的显着影响,减少受水文方案高度影响的区域中的SR流出。最后,从控制土壤二氧化碳排放的角度来看,我们建议当地政府应管理和引导河岸地区的农业活动。

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