摘要
以河北省围场县北沟林场内4种不同林分的枯落物层和土壤层为研究对象,对其水文效应进行初步研究。结果表明:(1)落叶松、油松混交林枯落物蓄积量最大,为12.28t/hm2,最大持水量为24.60t/hm2,有效拦蓄量为27.19t/hm2;油松林的枯落物蓄积量为11.74t/hm2,最大持水量为19.30t/hm2,有效拦蓄量为22.21t/hm2;落叶松林的枯落物蓄积量为9.32t/hm2,最大持水量为11.60t/hm2,有效拦蓄量为16.20t/hm2;落叶松白桦混交林的枯落物蓄积量为5.58t/hm2,最大持水量为12.90t/hm2,有效拦蓄量为13.53t/hm2。(2)半分解层枯落物浸泡8h已基本达到饱和,而未分解层需浸泡10h,通过分析得出持水量与浸泡时间的关系为Q=aln(t)+b;枯落物在浸水的前30min内吸水速率最大,6h左右时吸水速率明显减缓,枯落物吸水速率与浸泡时间的关系为V=ktn。(3)落叶松白桦混交林土壤层持水能力最强,为377.03t/hm2;落叶松油松混交林土壤层的持水能力最差,为241.9t/hm2,利用幂函数对入渗速率与入渗时间进行拟合,其相关系数均在0.95以上。
A pilot study of hydrological effect s of litters layer and soil layer was carried out in four kinds of forest stands in Beigou forest farm, Hebei province. The result showed: (1)The litter total storage capacity of Larix principis-rupprechti mixed Chinese pine was 12.28 t/hm^2 , the maximum water capacity was 24.60 t/hm^2, the modified interception amount was 27. 19 t/hm^2 ; the litter total storage capacity of Chinese pine was 11.74 t/hm^2, the maximum water capacity was 19. 30 t/hm^2, the modified interception amount was 22.21 t/hm^2 ; the litter total storage^2, capacity of Larix principis-rupprechti was 9.32 t/hm^2 , the maximum water capacity was 11.60 t/hm^2 , the modified interception amount was 16.20 t/hm2 ; the litter total storage capacity of Larix principis-rupprechti mixed white birch was 5.58 t/hm the maximum water capacity was 12.90 t/hm^2 , the modified interception amount was 13.53 t/hm2. (2)Semi-decomposition litter reached satu- ration in 8 h, and without-decomposition litter in 10 h, the relationship of water holding capacity and soaking time was Q=aln(t)+b; the absorption rate was the largest in first half-hour, after 6 h, the rate was obvi- ously slowed down and the relationship of absorption rate and soakperiod was V=kt". (3)The soil water holding capacity of Larix principis-rupprechti mixed white birch was the strongest to 377.03 t/hm^2, and Larix principis-rupprechti mixed Chinese pine was the worst to 241.9 t/hm^2 , using power function of infil- tration rate and infiltration fitting time, the correlation coefficient was above 0.95.
出处
《水土保持学报》
CSCD
北大核心
2011年第6期148-152,共5页
Journal of Soil and Water Conservation
基金
国家"十二五"科技支撑项目"海河上游水源涵养林体系构建技术研究与示范"(2011BAD38B05)
国家林业公益性行业科研专项"典型森林植被对水资源形成过程的调控研究"(201104005)
关键词
枯落物层
土壤物理性质
水文效应
litter layers soil physical property
hydrological effects