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红壤坡地不同土地利用方式下表层土壤活性碳、氮特征

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以红壤坡地长期定位试验(1995开始)为研究对象,研究自然林、草地、农作、油茶林和湿地松5种土地利用方式下表层土壤几种重要的活性碳、氮成分,包括无机态氮(NH4+-N、NO3-N)、可溶性有机碳、氮(DOC、DON)和微生物生物量碳、氮(MBC、MBN)含量及动态变化特征.结果表明,不同土地利用方式对坡地土壤DON含量没有显著影响(年均值在16.3~18.2mg/kg之间),土壤可溶性总氮(TDN)的差异主要来自可溶性无机氮(DIN).农作利用土壤NH4+-N、NO3-N含量显著高于其他利用方式,除油茶林外,其他土地利用方式NH+-N含量都高于NO3-N含量,其中自然林、草地利用方式下NH4+-N是NO3-N含量的2.2倍和11.8倍.不同坡地利用土壤MBC含量均值范围为195.7~437.2 mg/kg,土壤MBN含量为28.6~70.0 mg/kg,大小顺序为:草地区>自然林>湿地松>油茶林>农作区.土壤DOC年均值范围为237.3~290.7 mg/kg,其中草地土壤年均含量最高(290.7 mg/kg),显著高于其它4种利用方式.总体来看,除农作、油茶林土壤DOC≥MBC外,其他土地利用方式下土壤活性有机碳、氮成分均以MBC、MBN形态为主,土壤MBC/DOC和MBN/DON比值分别为1.1~1.6和1.7~3.9,其中草地土壤比值最大,农作土壤相差最小.土壤活性碳、氮含量与土壤有机碳、全氮含量关系并不密切,其含量可能受水土流失的影响.
Effects of Land Use Patterns on Active Carbon and Nitrogen of Red Soil in the Slope Land of Hilly Area
Characteristic of content and variation trends of soil inorganic nitrogen (NH4+-N,NO3--N),dissoluble organic carbon and nitrogen (DOC,DON)and microbial biomass carbon and nitrogen (MBC,MBN) were invested from topsoil of natural forest,grassland,farmland,sasanqua plantation and pinewoods in a long-term sloped land use experiment.The results showed that the five patterns did not have significantly effect on soil DON,the annual average of soil DON content varied from 16.3 mg/kg to 18.2 mg/kg,and the dissoluble inorganic nitrogen (DIN) in farmland soil was significantly higher than that in oher four of partterns.The content of soil NH4--N was higer than soil NO3--N in all land use patterns,except for sasanqua plantation.The content of MBC and MBN varied from 195.7 mg/kg to 437.2 mg/kg,and from 28.6 mg/kg to 70.0 mg/kg,respectively,and the order was farmland>grass land>natural forest>pinewoods>sasanqua plantation.In the whole,the main composition of soil active carbon and nitrogen were MBC,MBN,except for farmland and sasanqua plantation,which content of DOC was equal or higher lightly than MBC content.The rate of MBC to DOC and MBN to DON varied from 1.1 to1.6,and from 1.7 to 3.9 respectively,and it was highest for grassland,and lowest for farmland.The change of soil active carbon and nitrogen did not depend on the content of soil SOC and TN,which might be affected by the runoff of soil active carbon and nitrogen.

land use patternsinorganic nitrogendissolved organic carbon and nitrogenmicrobial biomass carbon and nitrogen

王飞、王卫、陈安磊、谢小立、李雁勇

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中国科学院亚热带农业生态研究所,亚热带农业生态过程重点实验室,长沙410125

中国科学院大学,北京100049

土地利用方式 无机态氮 可溶性有机碳、氮 微生物生物量碳、氮

国家自然科学基金公益性行业(农业)科研专项湖南省自然科学基金

3120033920120303008JJ3090

2014

水土保持学报
中国土壤学会 中国科学院水利部水土保持研究所

水土保持学报

CSTPCDCSCD北大核心
影响因子:1.226
ISSN:1009-2242
年,卷(期):2014.28(2)
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