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首页> 外文期刊>Journal of Forestry Research >Soil animals and nitrogen mineralization under sand-fixation plantations in Zhanggutai region, China
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Soil animals and nitrogen mineralization under sand-fixation plantations in Zhanggutai region, China

机译:张谷台地区固沙人工林下的土壤动物和氮矿化

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The effects of soil animals on soil nitrogen (N) mineralization and its availability were studied by investigating soil animal groups and their amounts of macro-faunas sorted by hand, and middle and microfaunas distinguished with Tullgren and Baermann methods under three Pinus sylvestris var. mongolica Litv. plantations in Zhanggutai sandy land, China. In addition, soil N mineralization rate was also measured with PVC closed-top tube in situ incubation method. The soil animals collected during growing season belonged to 13 orders, 5 groups, 4 phyla, whose average density was 86 249.17 individuals·m~(-2). There were significant differences in soil animal species, densities, diversities and evenness among three plantations. Permanent grazing resulted in decrease of soil animal species and diversity. The average ammonification, nitrification and mineralization rates were 0.48 g·m~(-2)·a~(-1), 3.68 g·m~(-2)·a~(-1) and 4.16 g·m~(-2)·a~(-1), respectively. The ammonification rate in near-mature forest was higher than that in middle-age forests, while the order of nitrification and net mineralization rates was: middle-age forest without grazing < middle-age forest with grazing < near-mature forest with grazing (P<0.05). Soil N mineralization rate increased with soil animal amounts, but no significant relationship with diversity. The contribution of soil animals to N mineralization was different for different ecosystems due to influences of complex factors including grazing, soil characteristics, the quality and amount of litter on N mineralization.
机译:通过调查土壤动物种类及其手工分选的大型动物群以及在三个樟子松下用Tullgren和Baermann方法区分的中型和小型动物群,研究了土壤动物对土壤氮(N)矿化及其有效性的影响。蒙古自治州中国张谷台沙地的人工林。另外,还采用PVC密闭管原位培养法测定了土壤氮的矿化率。生长季采集的土壤动物共13科5类4门,平均密度为86 249.17个人·m〜(-2)。三个人工林的土壤动物种类,密度,多样性和均匀性存在显着差异。永久放牧导致土壤动物种类和多样性减少。平均氨化,硝化和矿化速率分别为0.48 g·m〜(-2)·a〜(-1),3.68 g·m〜(-2)·a〜(-1)和4.16 g·m〜(- 2)·a〜(-1)。近成熟森林的氨化率高于中年森林,其硝化作用和净矿化率的顺序为:未放牧的中年森林<有放牧的中年森林<有放牧的近年森林( P <0.05)。土壤氮矿化率随土壤动物数量的增加而增加,但与多样性无明显关系。由于放牧,土壤特性,凋落物质量和数量等复杂因素对氮矿化的影响,不同生态系统中土壤动物对氮矿化的贡献不同。

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