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宁夏森林枯落物储量与持水性能分析
引用本文:马正锐,程积民,班松涛,赵凌平.宁夏森林枯落物储量与持水性能分析[J].水土保持学报,2012,26(4):199-203,238.
作者姓名:马正锐  程积民  班松涛  赵凌平
作者单位:1. 中国科学院水土保持与生态环境研究中心,陕西杨凌712100/中国科学院研究生院,北京100049
2. 中国科学院水土保持与生态环境研究中心,陕西杨凌,712100
3. 西北农林科技大学资源与环境学院,陕西杨凌,712100
4. 河南科技大学动物科技学院,河南洛阳,471003
基金项目:中国科学院战略性先导科技专项“应对气候变化的碳收支认证及相关问题”(XDA05050202);国家重点实验室基金项目(10502-Z8);林业公益性行业科研专项(200904056)
摘    要:采用野外实地调查与室内分析相结合的方法,对宁夏10种主要森林类型林下枯落物(未分解层和半分解层)储量、厚度、分解现状、持水率、吸水速率以及拦蓄量进行研究,并分析同一群落类型枯落物持水特性在不同区域的变化。结果表明:枯落物储量在1.06~76.49t/hm2之间,除辽东栎林外,针叶林蓄积普遍高于阔叶林;各森林类型枯落物的最大持水率,未分解层为117.82%~208.05%,半分解层为169.34%~302.85%,持水率随着浸泡时间的延长均按照对数方程增加;研究同一类型不同区域枯落物各层持水性能,发现宁夏范围内青海云杉林各层持水性能无明显差异,而小叶杨林下各层持水性能随区域、林龄的变化有显著变化,而华北落叶松林和油松林各样点都呈现未分解层差异显著,而半分解层差异较小的规律;各森林类型枯落物层的有效拦蓄量为0.11~10.27mm,且针叶林明显大于阔叶林。

关 键 词:枯落物  持水率  吸水速率  拦蓄量  宁夏

Litter Storage and Water-holding Characteristics of Typical Forest Types in Ningxia
MA Zheng-rui,CHENG Ji-min,BAN Song-tao,ZHAO Ling-ping.Litter Storage and Water-holding Characteristics of Typical Forest Types in Ningxia[J].Journal of Soil and Water Conservation,2012,26(4):199-203,238.
Authors:MA Zheng-rui  CHENG Ji-min  BAN Song-tao  ZHAO Ling-ping
Institution:1.Institute of Soil & Water Conservation and Eco-Environment,Chinese Academy of Sciences,Yangling,Shaanxi 712100;2.Graduate University,Chinese Academy of Science,Beijing 100049;3.College of Resources and Environment,Northwest A & F University,Yangling,Shaanxi 712100; 4.Animal Scienc and Technology School,Henan University of Science and Technology,Luoyang,Henan 471003)
Abstract:By using the methods of field investigation and soaking extraction,the storage,thickness,water-holding rate,water-absorption rate and interception of the litter in 10 forest types of Ningxia were studied,and changes of litter water-holding characteristics among different regions of the same vegetation also included.The results show that the amount of litters was 1.06~76.49 t/hm2,with a rank of conifer forest >broadleaved forest(except Quercus wutaishanica forest).The maximum water-holding rate of the un-decomposed layer ranged from 117.82% to 208.05%,and the half-decomposed layer ranged from 169.34% to 302.85%.These two parameters both increased with soaking time,following a logarithmic curve.The water-holding rate data of Picea crassifolia analysis revealed that there was no obvious difference in three places around Ningxia province,but the case of Populus simonii forest was opposite.Both Larix principis-rupprechtii and Pinus tabuliformis forest follow the law that the un-decomposed layer had a significant change while the half-decomposed layer show slight difference.And the water-absorption rate of both layers reached the maximum value in the first half an hour,slowed down obviously then.The modified interception ranged from 0.11~10.27 mm,followed the order of conifer forest >broadleaved forest.
Keywords:litter  water-holding rate  water-absorption rate  modified interception  Ningxia
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