形成湿地的“淹埋深-历时-频率”阈值研究进展  

Review on the study of “water stage-duration-frequency”thresholds for forming wetlands

作　　者：殷书柏[1] 沈方[1] 李子田[1] 付波霖 

机构地区：[1]唐山师范学院资源管理系,河北唐山063000 [2]中国科学院东北地理与农业生态研究所,吉林长春130102

出　　处：《水科学进展》2015年第4期596-604,共9页Advances in Water Science

基　　金：国家自然科学基金资助项目(41271113);河北省水利厅科研与推广计划项目(2014-058)~~

摘　　要：湿地水文是形成湿地的发生学因素,"淹埋深-历时-频率"(S,D,F)是表征湿地水文的特征指标。为了推进(S,D,F)阈值研究理论和方法的发展,总结了(S,D,F)阈值研究的一致结论:S阈值确定的原则是水饱和至地表;D阈值确定的原则是从水饱和开始到厌氧环境形成的时滞;F阈值应取≥50%。通过对这些一致结论的分析后认为:D阈值确定的原则存在着科学性问题;目前(S,D,F)阈值研究理论针对正常情况下湿地类型,不适合非正常情况下的湿地类型。为了科学地解决(S,D,F)阈值问题,必须构建新的(S,D,F)阈值确定的理论和方法,包括正常情况下和非正常情况(S,D,F)阈值确定的理论和方法以及(S,D,F)阈值科学性检验的理论和方法。Wetland hydrology is the driving force of wetland formation, ＂water stage-duration-frequency＂ （S, D, F） are the characteristic indexes of wetland hydrology. Aimed to promote the development of the theories and methods for determining （S, D, F） thresholds, the agreed conclusions derived from （S, D, F） threshold studies were summa- rized, which include： The principle of determining S threshold is ＂saturate to the earth＇s surface＂; the principle of determining D threshold is ＂the lag time from the onset of saturation to the formation of anaerobic condition＂ ; and F threshold should be I〉 50%. Through the analysis of these agreed conclusions, the results suggested： （1） There are sci- entific problems in using the principle of determining D threshold; （2） The present theories and methods for determi- ning （S, D, F） threshold were built for the wetlands of ＂normal condition＂, and can not be used to determine the （S, D, F） threshold of ＂abnormal condition＂. In order to get （S, D, F） thresholds scientifically, new scientific the- ories and methods for determining （S, D, F） threshold should be built, which should include： The （S, D, F） threshold theories and methods for wetlands of both ＂normal condition＂ and ＂abnormal condition＂, and the theories and methods of scientific testing for （S, D, F） thresholds.

关 键 词：湿地水文 “淹埋深-历时-频率”阈值 土壤水饱和 厌氧环境 

分 类 号：P343[天文地球—水文科学] G353.11[天文地球—地球物理学]