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Effect of Wetland Reclamation on Soil Aggregates Content and Soil Organic Carbon Distribution of Aggregates in Peat Mire Soil around Xingkai Lake in Northeast China

机译:湿地综合对中国东北兴凯湖周边泥炭泥土泥炭骨料含量及土壤有机碳分布的影响

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Soil aggregates content, soil organic carbon (SOC) concentration and density in soil aggregates in 0~5, 5~10, 10~20, 20~30 cm soil layers in peat mire soil in wetland, soybean and paddy field reclaimed from the wetland around Xingkai Lake were determined to investigate how reclamation of wetland for soybean and rice farming impacts soil aggregates content and SOC distribution of aggregates. After reclamation, >1 mm macro-aggregates decreased, 0.25~1mm macro-aggregates and micro-aggregates (0.053~0.25 mm and <0.053 mm) increased. In 0~5, 5~10, 10~20, 20~30 cm soil layers <0.25mm micro-aggregates content in soybean field were higher than in paddy filed by 10.18%, 11.2%, 3.35% and 13.13%, respectively. Wetland reclamation has reduced SOC concentration of aggregates and soil. SOC concentration in aggregates in soybean field was higher than in paddy field except in <0.053 mm micro-aggregates in 0~5 cm and 10~20 cm soil layers. SOC density in 0~30 cm soil layer was ordered from high to low as wetland>soybean field>paddy field. Due to reclamation, SOC density in <0.25 mm micro-aggregates in the four soil layers and its share in total soil SOC increased, and that in soybean field was higher than in paddy field. More SOC was allocated into <0.25mm micro-aggregates and might be protected better in soybean field than in paddy field, and reclaim the wetland into soybean field instead of paddy field is more beneficial for the long-term retention of SOC.
机译:土壤聚集含量,土壤有机碳(SoC)浓度和土壤聚集体中的密度在0〜5,5〜10,10〜20,20〜30cm土层中泥浆泥土中的湿地,大豆和稻田从湿地开垦决心在兴凯湖周围调查湿地为大豆和水稻农业影响的湿地影响土壤聚集含量和骨料分布。填海后,> 1mM宏观聚集体下降,0.25〜1mm宏观聚集体和微聚集体(0.053〜0.25mm,<0.053mm)增加。在0〜5,5〜10,10〜20,20〜30cm的土壤层<0.25mm微聚集在大豆田中的含量高于稻谷,分别归因于10.18%,11.2%,3.35%和13.13%。湿地填海综合减少了骨料和土壤的SoC浓度。除了0〜5cm和10〜20cm的土层中的0.053mm微聚集体中,大豆场聚集体中的SOC浓度高于稻田。 0〜30cm的土壤层中的SOC密度从高于低至低至湿地>大豆田>稻田。由于填海层,四层土壤层中<0.25mm微聚集体中的SOC密度及其在总土壤SOC中的份额增加,并且在大豆领域高于稻田。更多SOC被分配到<0.25mm的微聚集体中,并且在大豆场中可能比在稻田中更好地保​​护,并将湿地重新纳入大豆田而不是稻田对SOC的长期保留更有利。

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