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冻融对沼泽湿地土壤水稳性大团聚体的影响
引用本文:秦胜金,刘景双,丁洪,张玉树.冻融对沼泽湿地土壤水稳性大团聚体的影响[J].水土保持通报,2009,29(6):115-118.
作者姓名:秦胜金  刘景双  丁洪  张玉树
作者单位:秦胜金,QIN Sheng-jin(福建省农业科学研究院,土壤肥料研究所,福建,福州,350013;中国科学院,东北地理与农业生态研究所,吉林,长春,130012);刘景双,LIU Jing-shuang(中国科学院,东北地理与农业生态研究所,吉林,长春,130012);丁洪,张玉树,DING Hong,ZHANG Yu-shu(福建省农业科学研究院,土壤肥料研究所,福建,福州,350013) 
基金项目:福建省青年人才项目,国家自然科学基金,中国科学院知识创新工程重要方向项目 
摘    要:水稳性大团聚体(>0.25 mm)是土壤侵蚀和质量的重要表征指标.通过室内培养,在不同含水量、冻融次数和压实处理条件下,研究冻融过程对三江平原沼泽湿地土壤水稳性大团聚体的影响.结果表明,冻融过程影响土壤水稳性大团聚体含量,但压实和土壤起始含水量对湿地土壤的水稳性大团聚体影响较小,而冻融次数影响显著.4次冻融前,随着冻融次数的增加,不同处理的土壤水稳性大团聚体含量呈增加趋势;4次冻融后,高含水量处理的土壤水稳性大团聚体变化不明显,而低含水量处理的土壤水稳性大团聚含量有微弱增加.

关 键 词:冻融过程  水稳性大团聚体  沼泽湿地  三江平原
收稿时间:4/8/2009 12:00:00 AM
修稿时间:2009/5/25 0:00:00

Effects of Freezing2tha wing on Soil Water2stable Aggregates in Fresh Marsh
QIN Sheng-jin,LIU Jing-shuang,DING Hong and ZHANG Yu-shu.Effects of Freezing2tha wing on Soil Water2stable Aggregates in Fresh Marsh[J].Bulletin of Soil and Water Conservation,2009,29(6):115-118.
Authors:QIN Sheng-jin  LIU Jing-shuang  DING Hong and ZHANG Yu-shu
Institution:Institute of Soil and Fertilizer,Fujian Academy of Agricultural Sciences,Fuzhou,Fujian 350013,China;Northeast Institute of Geography and Agroecology,Chinese Academy of Sciences,Changchun,Jilin 130012,China;Northeast Institute of Geography and Agroecology,Chinese Academy of Sciences,Changchun,Jilin 130012,China;Institute of Soil and Fertilizer,Fujian Academy of Agricultural Sciences,Fuzhou,Fujian 350013,China;Institute of Soil and Fertilizer,Fujian Academy of Agricultural Sciences,Fuzhou,Fujian 350013,China
Abstract:Soil water-stable macro-aggregates (>0.25mm) are an important characteristic index of soil ero-sion and soil quality. The effects of freezing-thawing on the content of soil water-stable macro-aggregates in Sanjiang Plain wetlands were studied under different soil water contents,numbers of freezing2thaw cycles,and compaction treatments by indoor incubation experiment. Results showed that the content of soil water-stable macro-aggregate was influenced by the freezing2thawing. The effects of freezing-thawing frequency were more significant compared with compaction and initial soil water content. Before the 4th freezing-thaw cycle,the content of soil water-stable macro-aggregates under different treatments increased with the increas-ing of freezing2thawing frequency. After the 4th freezing-thaw cycle,however,the content at high soil water content did not change obviously and increased slightly.
Keywords:freezing-thawing  soil water-stable macro-aggregate  fresh mash  Sanjiang Plain
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