生态与农村环境学报 ›› 2015, Vol. 31 ›› Issue (5): 718-723.doi: 10.11934/j.issn.1673-4831.2015.05.016

• 自然保护与生态 • 上一篇    下一篇

水位对杭州湾芦苇湿地土壤有机碳、氮、磷含量的影响

盛宣才, 邵学新, 吴明, 宁潇, 叶小齐   

  1. 中国林业科学研究院亚热带林业研究所/国家林业局杭州湾湿地生态系统定位观测研究站
  • 收稿日期:2014-12-24 修回日期:2015-07-24 出版日期:2015-09-25 发布日期:2015-09-30
  • 通讯作者: 吴明 E-mail:hangzhoubay@126.com
  • 作者简介:盛宣才(1989-),男,合肥安徽人,硕士生,主要研究方向为湿地生态学。E-mail:sxcforest _08@126.com
  • 基金资助:

    国家科技支撑计划(2012BAC13B02);中国林科院基本科研业务费专项(CAFYBB2014MA002);国家林业公益性行业科研专项(201404210,201404305)

Effects of Water Level on Organic Carbon, Total Nitrogen and Total Phosphorus in Soil in Reed Wetlands of Hangzhou Bay

SHENG Xuan-cai,SHAO Xue-xin,WU Ming,NING Xiao,YE Xiao-qi   

  1. Research Institute of Subtropical Forestry, Chinese Academy of Forestry/Wetland Ecosystem Research Station of Hangzhou Bay,State Forestry Administration
  • Received:2014-12-24 Revised:2015-07-24 Online:2015-09-25 Published:2015-09-30

摘要:

为探明不同水位梯度对湿地土壤性质的影响,对杭州湾围垦芦苇湿地不同水位下土壤有机碳(SOC)、全氮(TN)、全磷(TP)含量和化学计量比及其相关性进行了研究。结果表明:(1)SOC和TN含量随着水位增加总体上均表现为先下降后升高的趋势,而TP沿水位梯度变化趋势不显著;(2)土壤未被水淹时(0cm水位)土壤C/P比、N/P比和C/N比均随土壤深度的增加而降低,而水淹后(10、20、30cm水位)土壤C/P比、N/P比和C/N比则呈现先降低后增加的趋势;(3)不同水位梯度SOC与N/P比、TN含量与C/P比均呈显著正相关(P<0.05),而土壤TP含量与C/N比呈负相关,但相关性不显著(P>0.05);(4)土壤pH值是影响杭州湾湿地0cm水位梯度下SOC、TN和TP含量变化的重要因子,但随着水位的增加土壤pH值与SOC、TN和TP含量的相关性逐渐减小。随着水位的增加,土壤深层的SOC和TN累积量逐渐增加,而土壤TP含量随水位增加趋势不明显;土壤pH值对SOC、TN和TP含量的影响随着水位的增加逐渐减弱。

关键词: 杭州湾湿地, 水位梯度, 有机碳, 全氮, 全磷, pH值

Abstract:

Water level in wetland may affect soil properties of the wetland.Effects of water level on soil properties of reed wetlands in Hangzhou Bay Polder were studied. The vertical distribution patterns of the soil organic carbon (SOC), total nitrogen (TN) and total phosphorus (TP) along the soil profile and their stoichiometric ratios relative to water level were investigated. Results show that: (1) on the whole, SOC and TN contents decreased at first then increased with rising water level, while the content of TP did not change much(P<0.05); (2) when the soil remained unsubmerged (Water level 0) C/P, N/P and C/N declined with soil depth, but when the soil was submerged, regardless of water levels, their initial decreases were followed by increases; (3) SOC was positively correlated with soil N/P and TN with soil C/P, while TP was negatively, but not so significantly with soil C/N at all water levels; and (4) soil pH was the major factor affecting SOC, TN and TP at 0cm water level, but the effect faded with rising water level. SOC and TN accumulations in the deep soil layers increased with rising water level, while TP did not change much(P<0.05).

Key words: Hangzhou Bay wetland, water level gradient, organic carbon, total nitrogen, total phosphorus, pH