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首页> 外文期刊>Journal of Hydrology >Impacts of natural wetland degradation on dissolved carbon dynamics in the Sanjiang Plain, Northeastern China
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Impacts of natural wetland degradation on dissolved carbon dynamics in the Sanjiang Plain, Northeastern China

机译:东北三江平原自然湿地退化对溶解碳动态的影响

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Wetlands are important dissolved organic carbon (DOC) reservoirs, and principal sources of DOC to the fluvial environment, constituting a significant linkage between land and ocean in the context of global carbon cycle. The Sanjiang Plain, a floodplain in Northeastern China that encompasses numerous natural freshwater wetlands, has been experiencing extensive building of drainage ditches and thus elevated degradation of wetlands. This paper investigated DOC, dissolved inorganic carbon (DIC), and dissolved total carbon (DTC) in soil, the surface ponding and rivers from natural wetlands and the degraded wetland, and also in an artificial drainage ditch in the Sanjiang Plain during the growing season (May to October) of 2009. Seasonal averaged DOC concentrations were greater in soil and the surface ponding of the degraded riparian wetland than those originating from the natural riparian wetlands (i.e. Bielahong, Yalv and Nongjiang riparian wetlands). Seasonal averaged DIC concentrations in the surface ponding of the degraded wetland increased by 1.76, 0.59 and 2.05 times, compared to those in the Bielahong, Yalv and Nongjiang riparian wetlands, respectively. Similar to dissolved carbon dynamics in the field sites, the seasonal averaged DOC concentration in the degraded marshy river showed higher value (10.36 ± 1.99. mg/L), compared to those in the pristine marshy rivers. Seasonal DIC concentrations followed a trend as the degraded marshy river (15.09 ± 2.43. mg/L) - the artificial ditch (12.52 ± 1.61. mg/L) - pristine marshy rivers on average (8.53 ± 0.96. mg/L). Seasonal mean DTC concentration in the artificial ditch showed higher values than that in the natural marshy rivers, while seasonal mean DTC concentration in the degraded marshy river was greater than that in the artificial ditch. Further, seasonal DOC and DIC dynamics were similar in the artificial ditch and the degraded marshy river. These qualitative changes in the dissolved carbon dynamics in our study might have important implications that the impact of building of artificial ditches on dissolved carbon of waters more fully reflected in increases of dissolved carbon resulting from wetland degradation rather than increases in the artificial ditch itself.
机译:湿地是重要的溶解有机碳(DOC)储集层,也是河流环境中DOC的主要来源,在全球碳循环的背景下,陆地和海洋之间有着重要的联系。三江平原是中国东北的洪泛区,周围有许多天然的淡水湿地,一直在建设大量的排水沟,从而加剧了湿地的退化。本文研究了土壤,自然湿地和退化湿地的表层池塘和河流以及生长期的三江平原人工排水沟中的DOC,溶解性无机碳(DIC)和溶解总碳(DTC)。 (2009年5月至10月)。退化的河岸湿地的土壤和表层池塘中的季节性平均DOC浓度要高于自然河岸湿地(即Bielahong,Yalv和Nongang河岸湿地)。与比拉红,雅绿和嫩江河岸湿地相比,退化湿地地表池中季节性平均DIC浓度分别增加了1.76、0.59和2.05倍。与田间站点的溶解碳动态相似,与原始沼泽河相比,退化的沼泽河的季节性平均DOC浓度更高(10.36±1.99。mg / L)。 DIC的季节性浓度呈趋势,即退化的沼泽河(15.09±2.43。mg / L)-人工沟(12.52±1.61。mg / L)-原始沼泽河的平均水平(8.53±0.96。mg / L)。人工沟渠中DTC的季节性平均浓度要高于天然沼泽河中的值,而退化泥泞河中DTC的季节性平均浓度要高于人工沟渠中的DTC浓度。此外,在人工沟渠和退化的沼泽河中,季节性DOC和DIC动态相似。在我们的研究中,溶解碳动力学的这些质的变化可能具有重要的含义,即人工沟渠对水体溶解碳的影响更充分地反映在湿地退化引起的溶解碳增加而不是人工沟渠本身的增加上。

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