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作 者:刘杏认[1] 董云社[1] 齐玉春[1] Manfred Domroes
机构地区:[1]中国科学院地理科学与资源研究所 [2]Institute of Geography,Mainz University,Mainz55099,Germany
出 处:《环境科学》2007年第3期633-639,共7页Environmental Science
基 金:国家重点基础研究发展规划(973)项目(2002CB412503);国家自然科学基金项目(40501072);中国科学院知识创新工程重大项目(KZCX1-SW-01-04);中国科学院地理科学与资源研究所知识创新项目(CXIOG-E01-03-01)
摘 要:应用树脂芯方法,研究了内蒙古锡林河流域不同降水强度3种草地类型土壤净氮矿化作用.结果表明,7~10月份,羊草草原的平均净氮矿化率为0.333kg.(hm2.d)-1,贝加尔针茅草原为0.316kg.(hm2.d)-1,克氏针茅草原为0.211kg.(hm2.d)-1;在相同的培养周期内,分阶段培养和连续培养对土壤的净氮矿化量和净氮矿化速率有显著影响;降雨是影响该区域氮素矿化的主要因素之一,3种草地类型土壤水分变化量与土壤净氮矿化速率呈正相关关系,相关系数分别为0.80、0.61、0.56.Soil net nitrogen mineralization rate of three types temperate grassland in Inner Mongolia, China was studied using the resin-core technique. The major results include: the net nitrogen mineralization rate of the Stipa baicalensis meadow grassland, the Aneulolepidum Chinense grassland and the Stipa krylovii grassland were 0.333 kg· ( hm^2· d) ^- 1 , 0.316 kg· ( hm^2 · d)^ - 1 and 0.211 kg · ( hm^2 · d) ^- 1 respectively during the field incubation period of July to October,2005; Soil net nitrogen mineralization accumulation and rates was remarkably different between phase incubation and continuous incubation during the same field incubation period ; Rainfall was one of the main factors affecting nitrogen mineralization. The net nitrogen mineralization rate was correlated with the change of soil moisture in all of the measured sites, the correlation coefficient was 0.80, 0.61 and 0.56.
分 类 号:X144[环境科学与工程—环境科学]
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