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Soil organic carbon of degraded wetlands treated with freshwater in the Yellow River Delta, China

机译:黄河三角洲经淡水处理的退化湿地土壤有机碳

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Supplying freshwater is one of the important methods to help restore degraded wetlands. Changes in soil properties and plant community biomass were evaluated by comparing sites with freshwater treatment versus reference sites following freshwater addition to wetlands of the Yellow River Delta for 7 years. The results indicated that soil organic carbon (SOC) was significantly increased in all wetland sites that were treated with freshwater compared to the reference sites. The treatment wetlands had greater total nitrogen (TN), lower pH and electrical conductivity and higher water content in the soil compared to the reference wetlands. In general, the upper soil layer (0-20 cm) had greater SOC than the lower soil layer (20—40 cm). The increase of SOC in the freshwater reintroduction wetlands was higher in the Suaeda salsa plant community (mean ± standard error) (6.89 ± 0.63 g/kg) and Phragmites communis plant community (4.11 ± 0.12 g/kg) than in the Tamarix chinensis plant community (1.40 ± 0.31 g/kg) in the upper soil layer. The differences were especially marked between the treated and reference wetlands for SOC and TN in the P. communis plant communities. The C:N ratio of the soil was significantly greater in the treated compared to the reference wetlands for the S. salsa plant community. Although the C: N ratios increased after treatment, they were all <25 suggesting that N availability was not limiting soil organic matter decomposition. Our results indicate that freshwater addition and the concomitant increase in soil moisture content enhances the accumulation of SOC in the Yellow River Delta.%School of Resources and Environment, University of Jinan, Jinan, Shandong 250022, PR China ,College of Life Science, Shandong University, Jinan, Shandong 250100, PR China ,State University of New York, College of Environmental Science and Forestry, Syracuse, NY 132W, USA;College of Life Science, Shandong University, Jinan, Shandong 250100, PR China ;College of Life Science, Shandong University, Jinan, Shandong 250100, PR China ;State University of New York, College of Environmental Science and Forestry, Syracuse, NY 132W, USA;State University of New York, College of Environmental Science and Forestry, Syracuse, NY 132W, USA;
机译:供应淡水是帮助恢复退化湿地的重要方法之一。通过将经过淡水处理的地点与参考地点相比,在黄河三角洲的湿地中添加淡水7年后,对土壤性质和植物群落生物量的变化进行了评估。结果表明,与参考地点相比,在所有用淡水处理过的湿地地点,土壤有机碳(SOC)均显着增加。与参考湿地相比,处理过的湿地具有更大的总氮(TN),较低的pH和电导率以及较高的土壤含水量。通常,上层土壤层(0-20 cm)的SOC大于下层土壤层(20-40 cm)。 Suaeda salsa植物群落(平均值±标准误差)(6.89±0.63 g / kg)和Phragmites communis植物群落(4.11±0.12 g / kg)的淡水再引入湿地中SOC的增加均高于Tamarix chinensis植物上部土壤层中的生物群落(1.40±0.31 g / kg)。在经过处理的湿地和参考湿地之间,P。communis植物群落中的SOC和TN之间的差异尤为明显。与S. salsa植物群落的参考湿地相比,处理后的土壤的C:N比明显更高。尽管处理后碳氮比增加,但均<25,表明氮的有效利用并不限制土壤有机质的分解。我们的研究结果表明,增加淡水和土壤水分的同时增加,增加了黄河三角洲土壤有机碳的积累。%暨南大学资源与环境学院,山东济南250022,生命科学学院,山东大学,山东济南250100,美国纽约州立大学环境科学与林业学院,纽约锡拉丘兹,纽约132W;山东大学生命科学学院,山东济南250100;中国生命科学学院,山东大学,山东济南250100;纽约州立大学,美国锡拉丘兹市环境科学与林业学院,纽约132W;纽约州立大学,美国锡拉丘兹市环境科学与林业学院,纽约132W,美国;

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