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川西亚高山针阔混交林与针叶纯林苔藓凋落物层持水性能研究
引用本文:郭伟,文维全,黄玉梅,张健,张丹桔,刘洋,刘旭,王伟.川西亚高山针阔混交林与针叶纯林苔藓凋落物层持水性能研究[J].水土保持学报,2009,23(6).
作者姓名:郭伟  文维全  黄玉梅  张健  张丹桔  刘洋  刘旭  王伟
作者单位:1. 四川农业大学林业生态工程省级重点实验室,四川,雅安,625014
2. 阿坝州川西林业局,四川,阿坝州,623102
基金项目:国家科技支撑计划,四川农业大学创新团队计划
摘    要:采用野外实地观测和室内浸水法对川西亚高山地区针阔混交林与针叶纯林林下苔藓凋落物的持水能力进行了对比研究.结果表明:(1)混交林林下苔藓凋落物层储量为10.02 t/hm~2,最大平均持水量为54.96 t/hm~2,最大平均持水率为839.70%;苔藓储量为2.43 t/hm~2,最大平均持水量为11.47 t/hm~2,最犬平均持水率为472.23%,吸水速率经过24 h从7 683.2 g/(kg·h)下降为256.5 g/(kg·h);凋落物储量为7.59 t/hm~2,最大平均持水量为24.07t/hm~2.最大平均持水率为317.22%.吸水速率经过24 h从8 530.1 g/(kg·h)下降为321.4 g/(kg·h).(2)针叶纯林林下苔藓凋落物层储量为9.37t/hm~2,最大平均持水量为45.70 t/hm~2,最大平均持水率为766.05%;苔藓储量为2.13 t/hm~2,最大平均持水量为9.68 t/hm~2,最大平均持水率为454.85%.吸水速率经过24 h从6 444.4 g/(kg·h)下降为231.4 g/(kg·h);凋落物储量为7.24 t/hm~2,最大平均持水量为21.20 t/hm~2,最大平均持水率为292.68%,吸水速率经过24 h从7 004.9 g/(kg·h)下降为251.4 g/(kg·h).因此,无论是持水量、持水率,还是吸水速率,混交林都强于针叶纯林.两种林分下,苔藓、凋落物持水率随浸泡时间的增加而增加,持水率与浸泡时间呈对数关系;苔藓、凋落物的吸水速率随浸泡时间的增加而降低,吸水速率与浸泡时间呈幂函数关系.

关 键 词:川西亚高山  苔藓  凋落物  持水性能

Water Holding Capacities of Bryophyte and Litter Layer Under Mixed Forest and Coniferous Forest in Subalpine Region of Western Sichuan
GU Wei,WEN Wei-quan,HUANG Yu-mei,ZHANG Jian,ZHANG Dan-ju,LIU Yang,LIU Xu,WANG Wei.Water Holding Capacities of Bryophyte and Litter Layer Under Mixed Forest and Coniferous Forest in Subalpine Region of Western Sichuan[J].Journal of Soil and Water Conservation,2009,23(6).
Authors:GU Wei  WEN Wei-quan  HUANG Yu-mei  ZHANG Jian  ZHANG Dan-ju  LIU Yang  LIU Xu  WANG Wei
Abstract:By field survey and water immersion,water holding capacities of bryophyte and litter layer under mixed forest and coniferous forest in sub-alpine region of western Sichuan were studied.The results showed that:(1)In the mixed forest,the storage amount bryophyte and litter layer was 10.02 t/hm~2,the maximal water holding capacity was 54.96 t/hm~2,the average mean maximal water holding rate was 839.70%, Bryophyte storage amount was 2.43 t/hm~2,the maximal water holding capacity was 11.47 t/hm~2,the maximal water holding rate was 472.23%,and the water absorption rate decreased from 7683.2 g/(kg·h)to 256.5 g/(kg·h)after 24 h;litter storage amount was 7.59 t/hm~2,the maximal water holding capacity was24.07 t/hm~2,the maximalwater holding rate was 317.22 %,the water absorption rate decreased from 8530.1 g/(kg·h)to 321.4 g/(kg·h)after 24h.(2)In the coniferous forest,bryophyte and litter layer storage amount was 9.37 t/hm~2,the maximal water holding capacity was 45.07 t/hm~2,the maximal water holding rate was 766.05%;Bryophyte storage amount was 2.13 t/hm~2,the maximal water holding capacity was 9.68 t/hm~2,the maximal water holding rate was 454.85%,and after 24h,the water absorption rate decreased from 6444.4 g/(kg·h)to 231.4 g/(kg·h);while,litter storage amount was 7.24 t/hm~2,the maximal water holding capacity was 21.20 t/hm~2,the maximal water holding rate was 292.68%,and after 24h,the water absorption rate decreased from 7004.9 g/(kg·h)to 251.4 g/(kg·h).Therefore,on the aspects of water holding capacity,water holding rate,or water absorption rate,the mixed forest was always higher than coniferous forest.Water holding rate of bryophyte and litter in the two kinds of forest increased logarithmically with time immersed in water;while water absorption rate decreased with the increasing time,representing power function trend.
Keywords:sub-alpine region of western Siehuan  bryophyte  litter  water holding capacity
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