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封育年限对伊犁绢蒿荒漠土壤有机氮组分的影响
引用本文:杨静,孙宗玖,董乙强.封育年限对伊犁绢蒿荒漠土壤有机氮组分的影响[J].草业科学,2017,34(9).
作者姓名:杨静  孙宗玖  董乙强
作者单位:1. 新疆农业大学草业与环境科学学院,新疆乌鲁木齐,830052;2. 新疆农业大学草业与环境科学学院,新疆乌鲁木齐830052;新疆草地资源与生态自治区重点实验室,新疆乌鲁木齐830052
基金项目:国家自然科学基金——不同退化蒿类荒漠土壤有机碳组及其碳氮特征对禁牧的响应
摘    要:为探究荒漠土壤有机氮组分对封育年限的响应规律,研究了不同封育年限(封育时间为0、1、4和11a)对中度退化伊犁绢蒿(Seriphidium transiliense)荒漠草地土壤全氮(total nitrogen,TN)、轻组氮(light fraction organic nitrogen,LFON)、颗粒氮(particulate organic nitrogen,PON)、微生物量氮(soil microbial biomass nitrogen,SMBN)及其分配比例的影响。结果表明,与封育0a相比,其它封育年限5-10、10-20、30-50cm土层的TN含量均显著降低(P0.05),且0-50cm土层TN含量随封育年限延长呈"降-升"趋势;封育11a,0-5cm土层PON含量达到最高,而封育4a,5-10和20-30cm土层PON分配比例显著增加;0-20cm土层LFON含量增加显著,且0-5cm土层含量最高。0-50cm土层SMBN随封育年限增加呈"降-升"趋势,而封育4a,5-10和20-30cm土层SMBN分配比例显著高于封育0a和封育1a(P0.05);0-10cm土层LFON和0-50cm土层LFONR与封育年限呈显著正相关。总之,短期封育(1~11a)下,中度退化伊犁绢蒿荒漠土壤全氮含量仍未得到恢复,但促进了LFON、PON、SMBN及其分配比例的增加。

关 键 词:封育年限  伊犁绢蒿荒漠  土壤颗粒氮  轻组氮  微生物生物量氮

Effects of grazing exclusion length on soil organic nitrogen in Seriphidium transiliense desert
Yang Jing,Sun Zong-jiu,Dong Yi-qiang.Effects of grazing exclusion length on soil organic nitrogen in Seriphidium transiliense desert[J].Pratacultural Science,2017,34(9).
Authors:Yang Jing  Sun Zong-jiu  Dong Yi-qiang
Abstract:To explore the effects of different grazing exclusion lengths on soil organic nitrogen,we studied total soil nitrogen,particulate organic nitrogen,light fraction organic nitrogen,soil microbial biomass nitrogen and their distribution ratios in a moderately degraded Seriphidium transiliense desert.The influence of different grazing exclusionlengths on the percentage of soil organic nitrogen was researched using a control,one grazingexclusion year,four grazing-exclusion years and eleven grazing-exclusion years.Compared with the control,the content of total soil nitrogen significantly decreased in 5-10,10-20 and 30-50 cm of soil depth and the content of total nitrogen in 0-50 cm of soil depth appeared first to decrease then increased with the increase in grazing-exclusion years.The particulate organic nitrogen was highest in 0-5 cm of soil depth after eleven grazing-exclusion years,with a significant increase in the accumulation of particulate organic nitrogen distribution ratios in soil depths of 5-10 and 20-30 cm.Light fraction organic nitrogen significantly increased in 0-20 and 0-5 cm of soil depth,while it reached the highest after four grazing-exclusion years.The soil microbial biomass nitrogen appeared first to decrease then increased in 0-50 cm of soil depth.Comparing four grazing-exclusion years with the control and one grazing-exclusion year,soil microbial biomass nitrogen distribution ratio significantly increased in 5-10 cm and 20-30 cm of soil depth.Correlation among grazing-exclusion years with light fraction organic nitrogen in 0-10 cm of soil depth and light fraction organic nitrogen distribution ratio in 0-50 cm of soil depth was significantly positive.In conclusion,the content of total soil nitrogen was not recovered,but light fraction organic nitrogen,particulate organic nitrogen,soil microbial biomass nitrogen and their distribution ratios increased after short-term grazing exclusion (1 ~ 11 a) in moderately degraded S.transiliense desert.
Keywords:grazing exclusion length  Seriphidium transiliense desert  soil particulate organic nitrogen  light fraction organic nitrogen  soil microbial biomass nitrogen
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