[1]何琴飞,彭玉华,侯远瑞,等. 珠江中游几种林地涵养水功能的调查分析[J].西北林学院学报,2017,32(1):48-53.[doi:10.3969/j.issn.1001-7461.2017.01.08]
 HE Qin-fei,PENG Yu-hua,HOU Yuan-rui,et al. Investigation and Analysis of Water Conservation Function of Several Forest Types in the Middle Reaches of Pearl River[J].JOURNAL OF NORTHWEST FORESTRY UNIVERSITY,2017,32(1):48-53.[doi:10.3969/j.issn.1001-7461.2017.01.08]
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 珠江中游几种林地涵养水功能的调查分析()
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《西北林学院学报》[ISSN:1001-7461/CN:61-1202/S]

卷:
第32卷
期数:
2017年第1期
页码:
48-53
栏目:
出版日期:
2017-01-31

文章信息/Info

Title:
 Investigation and Analysis of Water Conservation Function of Several Forest Types in the Middle Reaches of Pearl River
文章编号:
1001-7461(2017)01-0048-06
作者:
 何琴飞123彭玉华123侯远瑞123申文辉123*何峰123
 (1.广西林业科学研究院,广西 南宁 530002;2.广西优良用材林资源培育重点实验室,广西 南宁 530002;3.国家林业局 中南速生材繁育实验室,广西 南宁 530002)
Author(s):
 HE Qin-fei123PENG Yu-hua123HOU Yuan-rui123SHEN Wen-hui123*HE Feng123
 (1.Guangxi Academy of Forestry,Nanning,Guangxi 530002,China; 2.Guangxi Key Laboratory of Superior Timber Trees Resource Cultivation,Nanning,Guangxi 530002,China; 3.Key Laboratory of Central South Fast-growing Timber Cultivation,Nanning,Guangxi 530002,China)
关键词:
 珠江林地类型保持水分功能
Keywords:
 Pearl River forest types holding water function
分类号:
S715.7
DOI:
10.3969/j.issn.1001-7461.2017.01.08
文献标志码:
A
摘要:
 通过野外样地调查与室内浸水试验相结合的方法,调查分析了珠江中游苍梧县境内的5种林地类型的灌草层、凋落物层、土壤层的涵养水功能。结果表明:1)5种林地林下灌草本层的生物量为1.00~5.14 t·hm-2;持水量为2.65~19.54 t·hm-2,大小顺序为桉树林>湿地松+荷木混交林>马尾松林>大叶栎林>红锥林,与其生物量的变化规律基本一致;2)凋落物的累积量为7.71~40.18 t·hm-2,持水量为13.12~77.09 t·hm-2,大小顺序为湿地松+荷木混交林>桉树林>马尾松林>大叶栎林>红锥林,与累积量的大小顺序基本一致;3)土壤容重随土层的增加而增大,非毛管孔隙度、毛管孔隙度、总孔隙度分别为1.59%~7.93%、40.63%~50.50%、44.39%~52.32%,60 cm土层厚度的土壤持水量为2 663.08~3 207.86 t·hm-2,大小顺序为红锥林>湿地松+荷木混交林>桉树林>大叶栎林>马尾松林,与总孔隙度变化规律一致;4)不同林地林下层总持水量为2 684.91~3 223.63 t·hm-2,大小顺序与土壤持水量的顺序一致,且不同层次持水能力为土壤层>凋落物层>灌草层。
Abstract:
 By the method of combining field investigation and immersion test,the water conservation functions of three levels (shrub and grass,litter ,and soil level) under five forests (Pinus massoniana,Eucalyptus ,Castanopsis hystrix,Quercus griffithii,mixed P.elliottii + Schima superba) in the middle reaches of Pearl River,were quantitatively analyzed.The results indicated 1) in the shrub and grass layer,the biomass was 1.00-5.14 t·hm-2,and the maximum water-holding capacity varied from 2.65 to 19.54 t·hm-2 in the order of Eucalyptus>P.elliottii+S.superba>P.massoniana>C.hystrix>Q.griffithii forest.2) In the litter layer,the accumulation amount was 7.71-40.18 t·hm-2,the maximum water-holding capacity raged from 13.12 to 77.09 t·hm-2 in the order of P.elliottii+S.superba>Eucalyptus>P.massoniana>C.hystrix>Q.griffithii forest.3) Soil bulk density increased with the increase of soil depth.Soil non-capillary porosity,capillary porosity and total porosity ranged 1.59%-7.93%,40.63%-50.50% and 44.39%-52.32%,respectively.The maximum water-holding capacity of 60 cm soil layer raged 2 663.08-3 207.86 t·hm-2 in the order of C.hystrix>P.elliottii+S.superba>Eucalyptus>Q.griffithii>P.massoniana forest.4) The maximum water-holding capacity under forests was between 2 684.91 and 3 223.63 t·hm-2,and the order was the same as the soil.The maximum water-holding capacity of soil layer was higher than the litter layer,the lowest one was the shrub and grass layer.

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备注/Memo

备注/Memo:
 收稿日期:2016-04-13修回日期:2016-06-03
基金项目:国家林业公益性行业科研专项(201204512);“十二五”广西林业科技项目(桂林科字[2012]第7号)。
作者简介:何琴飞,女,工程师,硕士,研究方向:森林生态。E-mail:dragonfly.hqf@126.com
*通信作者:申文辉,男,教授级高工,在读博士,研究方向:森林生态、森林培育。E-mail:shenwenhui2003@163.com
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