Nitrogen Characteristics of Peatland Under Different Degradation States in Gahai Lake Wetland of South Gansu Province
Author:
  • Article
  • | |
  • Metrics
  • |
  • Reference [28]
  • |
  • Related [20]
  • |
  • Cited by
  • | |
  • Comments
    Abstract:

    [Objective] The objective of the study is to analyze the variation of peat soil nitrogen under different degradation states in Gahai lake in South Gansu Province and provide scientific basis for peatland ecological restoration and protection in Gahai lake.[Methods] Through field sampling and laboratory analysis, we studied the changes in surface soil nitrogen(0-40 cm) of peat land with degradation.[Results] Except for the undegraded peat land, the total nitrogen content of the other 3 types of degraded peat land was significantly higher in September than that in July, while the soil C/N ratio and soil total nitrogen change in an opposite direction. The change in the content of ammonium nitrogen in soil was the same in July and September. The soil available nitrogen in the 0-20 cm layer was significantly higher in September than that in July, and the 20-40 cm layer(except for moderate degradation) was the opposite. In the whole profile, total soil nitrogen, soil C/N ratio and available nitrogen content were enriched in 20-40 cm layer. Except for moderate degradation, soil ammonium nitrogen was enriched in the 0-20 cm layer.[Conclusion] The total nitrogen content of 4 kinds of degraded soil has obvious temporal variation, indicating that the vegetation plays an important role in the recovery of peatland in Gahai lake.

    Reference
    [1] 李菊梅,王朝辉,李生秀.有机质、全氮和可矿化氮在反映土壤供氮能力方面的意义[J].土壤学报,2003,40(2):232-238.
    [2] 白军红,李晓文,崔保山,等.湿地土壤氮素研究概述[J].土壤,006,38(2):143-147.
    [3] 张昆,田昆,吕宪国,等.纳帕海湖滨草甸湿地土壤氮动态对水文周期变化的响应[J].环境科学,2009,30(8):2216-2220.
    [4] 范桥发,肖德荣,田昆,等.不同放牧对滇西北高原典型湿地土壤碳,氮空间分布的差异影响[J].土壤通报,2014,45(5):1151-1156.
    [5] 焦立恒.典型滨河湿地植被恢复过程中氮素变化特征研究[D].河南焦作:河南理工大学,2012.
    [6] 张金波,宋长春,杨文燕.三江平原不同土地利用方式下碳,氮的动态变化[J].吉林农业大学学报,2003,25(5):548-550.
    [7] 石福臣,李瑞利,王绍强.三江平原典型湿地土壤剖面有机碳及全氮分布与积累特征[J].应用生态学报,2007,18(7):1425-1431.
    [8] 蔡倩倩,郭志华,胡启鹏,等.若尔盖高寒嵩草草甸湿地不同水分条件下土壤有机碳的垂直分布[J].林业科学,2013,49(3):9-16.
    [9] 王元峰,王辉,马维伟,等.尕海湿地泥炭土土壤理化性质[J].水土保持学报,2012,26(3):118-122.
    [10] 张宁,冯磊,张迎梅.基于RS和GIS技术的尕海湿地景观变化趋势分析[J].甘肃林业科技,2011,36(1):10-14.
    [11] 徐鹏彬,邓建明,赵长明.甘肃尕海湿地不同海拔草地群落组分及物种多样性研究[J].草业学报,2012,21(2):219-227.
    [12] 虎高勇,李俊臻.甘肃尕海湿地及其生物多样性特征[J].甘肃林业科技,2011,36(3):24-28.
    [13] 王元峰.尕海湿地土壤水分物理特性研究[D].兰州:甘肃农业大学,2012.
    [14] 马维伟,王辉,黄蓉,等.尕海湿地生态系统土壤有机碳储量和碳密度分布[J].应用生态学报,2014,25(3):738-744.
    [15] 王元峰,王辉,马维伟,等.尕海湿地泥炭土土壤理化性质[J].水土保持学报,2012,26(3):118-122.
    [16] 黄蓉.尕海洪泛湿地退化过程中土壤理化性质的变化特征研究[D].兰州:甘肃农业大学,2014.
    [17] 刘育红,李希来,李长慧,等.三江源区高寒草甸湿地植被退化与土壤有机碳损失[J].农业环境科报,2009,28(12):2559-2567.
    [18] 鲁如坤.土壤农业化学分析方法[M].北京:中国农业科技出版社,1999.
    [19] 马雪华.森林生态系统定位研究方法[M].北京:中国科学技术出版社,1994.
    [20] 王玲玲,孙志高,牟晓杰,等.黄河口滨岸潮滩不同类型湿地土壤氮素分布特征[J].土壤通报,2011,42(6):1439-1445.
    [21] 张金屯.全球气候变化对自然土壤碳,氮循环的影响[J].地理科学,1998,18(5):463-471.
    [22] 余晓鹤,朱培立,黄东迈,等.土壤表层管理对稻田土壤氮矿化势,固氮强度及铵态氮的影响[J].中国农业科学,1991,24(1):73-79.
    [23] 白军红,邓伟,张玉霞.内蒙古鸟兰泡湿地环带状植被区十壤有机质及全氮空间分异规律[J].湖泊科学,2002,14(2):145-15.
    [24] 董云霞.纳帕海湿地区土壤碳氮要素分异特征研究[D].昆明:云南大学,2011.
    [25] 万晓红,王雨春,陆瑾,等.白洋淀湿地氮素转化和N2O排放特征研究[J].水利学报,2009,7(10):1168-1174.
    [26] 王常慧.内蒙古温带典型草原土壤净氮矿化作用[D].北京:中国科学院研究生院植物研究所,2005.
    [27] 闫琴.黄河口湿地土壤氮素的季节动态变化及转化过程研究[D].山东青岛:中国海洋大学,2010.
    [28] Chapin Ⅲ F S, Matson P A, Mooney H A. 陆地生态系统生态学原理[M].李博,赵斌,彭容豪,译.北京:高等教育出版社,2005.
    Cited by
    Comments
    Comments
    分享到微博
    Submit
Get Citation

吴江琪,马维伟,李广.甘南尕海湿地泥炭地不同退化状态下氮素的特征[J].水土保持通报英文版,2016,36(5):107-112

Copy
Share
Article Metrics
  • Abstract:1135
  • PDF: 1216
  • HTML: 0
  • Cited by: 0
History
  • Received:October 17,2015
  • Revised:December 22,2015
  • Online: November 22,2016