| 冻融交替对河岸缓冲带土壤无机氮和土壤微生物量氮的影响 |
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| 引用本文： | 范志平,李胜男,李法云,高洪翠,闫加亮.冻融交替对河岸缓冲带土壤无机氮和土壤微生物量氮的影响[J].气象与环境学报,2013,29(4):106-112. |
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| 作者姓名： | 范志平 李胜男 李法云 高洪翠 闫加亮 |
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| 作者单位： | 1.辽宁石油化工大学生态环境研究院，辽宁 抚顺 113001；2.中国科学院沈阳应用生态研究所，辽宁 沈阳 110016；3.中国科学院研究生院，北京 100049 |
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| 基金项目： | "十二五"国家科技支撑计划项目，"十二五"国家重大科技水专项，辽宁石油化工大学科技创新人才引进团队计划共同资助 |
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| 摘 要： | 全球气候变化引起的中高纬度地区积雪覆盖和降雪格局变化，造成该区域土壤冻融交替强度和频次变化，是土壤氮循环的重要影响因素。冻融温差和冻融循环次数影响微生物数量和群落的变化，进而影响土壤氮素生物地球化学循环。以大伙房水库实验林场小流域的河岸缓冲带生态系统为研究对象，通过分析冻融交替对河岸缓冲带土壤无机氮和土壤微生物量氮的影响，阐明冻融交替对土壤无机氮含量变化的影响机制，为评估小流域氮素流失风险提供依据。结果表明：随着冻融循环次数的增加，土壤无机氮含量呈增加趋势；不同温差的冻融循环处理对土壤无机氮影响不同，冻融条件为-5/+5℃和-20/+5℃时土壤无机氮含量在冻融循环10次之后分别为34.9±0.9 mg/kg和37.2±0.8 mg/kg，是处理前的1.21和1.41倍；冻融温差和冻融循环次数对土壤NH4+–N含量有极显著影响(P<0.01)，土壤冻融10次后土壤NH4+–N含量是对照处理的4-10倍；冻融循环次数对土壤NO3－–N含量有显著影响(P<0.05)，冻融温差对NO3－–N含量无显著影响(P>0.05)；土壤微生物量氮含量对冻融循环的响应显著(P<0.01)。可见，冻融交替显著增加了土壤无机氮含量，由于早春季节植被对无机氮吸收较少，可能增大土壤氮素随冰雪融化的淋溶流失风险。
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| 关 键 词： | 冻融交替 无机氮 土壤微生物量氮 河岸缓冲带 小流域 |
Effect of freezing-thawing on soil dissolved inorganic nitrogen and soil microbial biomass nitrogen in riparian zone |
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| FAN Zhi-ping
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LI Sheng-nan
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LI Fa-yun
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GAO Hong-cui
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YAN Jia-Liang.Effect of freezing-thawing on soil dissolved inorganic nitrogen and soil microbial biomass nitrogen in riparian zone[J].Journal of Meteorology and Environment,2013,29(4):106-112. |
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| Authors: | FAN Zhi-ping LI Sheng-nan LI Fa-yun GAO Hong-cui YAN Jia-Liang |
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| Institution: | 1. Institute of Eco-environment Sciences, Liaoning Shihua University, Fushun 113001, China; 2. Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; 3. Graduate University of Chinese Academy of Sciences, Beijing 100049, China |
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| Abstract: | Changes of intensity and frequency of soil freezing-thawing cycles are important factors affecting the N cycle in the riparian ecosystem in eastern mountain of Liaoning province. The freezing-thawing cycles could affect soil nitrogen cycles through microbial biomass and community. The study was carried out in Dahuofang experimen- tal forest watershed. The effect mechanism of freezing-thawing cycles on inorganic nitrogen content of soil was re- vealed, which could provide the references for assessing the risk of N loss in the riparian ecosystem. The results show that soil inorganic nitrogen content is in an increasing trend with the increasing times of freezing-thawing cy- cles. Different freezing temperature has the significant effect on inorganic nitrogen. The inorganic nitrogen contents are 34. 9 -0. 9 mg.kg-1 and 37. 2-0. 8 mg-kg-1 after 10 freezing-thawing cycles with the -5℃/＋5℃ and -20 ℃/＋5 ℃ treatments,which are 1.21 and 1.41 times of initial inorganic nitrogen content of soil samples,re- spectively. Furthermore, freezing-thawing cycles and its temperature difference have the significant effect on soil NH4-N content （P 〈0. 01 ）. After 10 freezing-thawing cycles, soil NH4＋ -N content is 4-10 times of soil samples for ＋ 5 ℃treatment. Freezing-thawing cycles have the significant influences on soil NO3- -N content （ P 〈 0. 05 ）, while its temperature difference has not the significant influences on NO3--N content（ P 〉 0. 05 ）. The response of soil microbial biomass nitrogen content to freezing-thawing cycles is significant（ P 〈 0.01 ）. |
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| Keywords: | Freezing-thawing change Inorganic nitrogen Microbial biomass nitrogen of soil Riparian zone Small watershed |
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