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作 者:陈书信 王国兵[1] 阮宏华[1] 岳臻[1] 徐长柏 徐亚明
机构地区:[1]南京林业大学,江苏省林业生态工程重点实验室,江苏南京210037 [2]江苏省东台市国有林场,江苏东台224200
出 处:《南京林业大学学报(自然科学版)》2014年第1期41-46,共6页Journal of Nanjing Forestry University:Natural Sciences Edition
基 金:国家林业公益性行业科研专项项目(201104006)
摘 要:土壤氮矿化速率常被作为生态系统中氮有效性和氮损失的指标。不同的土地利用方式可能影响土壤氮素的矿化、运输和植物的吸收与利用,因而造成土壤氮素循环过程的差异。该研究以苏北沿海地区杨树纯林、杨农复合、草地和农田等4种不同土地利用模式为研究对象,采用原位封顶法测定了土壤矿质氮含量的变化,分析了不同土地利用方式土壤氮净矿化速率的特征,以及土壤矿质氮与土壤微生物量氮(SMBN)、土壤水溶性有机氮(WSON)与土壤主要理化性质的相关关系。结果表明:不同土地利用方式土壤净矿化速率从大到小表现为杨树纯林〉杨农复合〉农田〉草地;土壤铵态氮(NH﹢4-N)与N矿化速率、SMBN、全氮有显著的正相关(p〈0.05);土壤硝态氮(N03一N)与SMBN、WSON、有机碳有极显著的正相关(p〈0.01);NH。’一N、矿质总氮(TMN)与土壤C/N有极显著的负相关(p〈0.01)。土壤矿质氮含量随土层的加深而显著减少;在〉10~25cm土层,杨树纯林与杨农复合之间的土壤矿质氮含量差异显著(p〈0.05)。研究结果表明土地利用方式的改变将影响土壤氮净矿化速率,森林转变为农田或农林复合结构后.氮在土壤中的储量和循环遗率瞳著降低。In order to study the effect of different land use patterns on soil N mineralization, transportation, absorption and utilization of plant, and which lead to difference of soil nitrogen cycle, we selected four different land use patterns (i.e. poplar plantation, crop-poplar integrated system, meadow and cropland) in a coastal area of northern Jiangsu as the experimental sites. The variations of soil mineral N were determined by close-top incubation method. The soil net N mineralization rate, soil microbial biomass nitrogen ( SMBN), water-soluble organic nitrogen (WSON) and soil physical and chemical properties were analyzed. The resuhs showed that the net N mineralization rate decreased in order of poplar plantation, crop-poplar integrated system, cropland and meadow. Ammonium N was significantly positive correlated with microbial biomass nitrogen and total nitrogen, the nitrate N was significantly positive correlated with microbial biomass nitrogen, WSON and organic carbon, but the soil C/N was significantly negative correlated with ammonium N and total mineral nitrogen. The soil mineral nitrogen decreased with soil depth increasing. In 25-40 cm soil layers, the soil miner- al nitrogen had significant difference with poplar plantation and crop-poplar integrated system. The results indicated that different land use patterns would affect soil net N mineralization rate, and the conversion of forest into cropland or crop- forest system could also alter the cycle rate of nitrogen significantly.
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