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大兴安岭山地樟子松天然林土壤水分物理性质及水源涵养功能研究
引用本文:李奕,满秀玲,蔡体久,盛后财.大兴安岭山地樟子松天然林土壤水分物理性质及水源涵养功能研究[J].水土保持学报,2011,25(2):87-91,96.
作者姓名:李奕  满秀玲  蔡体久  盛后财
作者单位:东北林业大学林学院,哈尔滨,150040
基金项目:林业公益性行业科研专项(201104005-05); 东北林业大学研究生论文资助项目(STIP10)
摘    要:对大兴安岭山地樟子松天然林土壤水分物理性质及水源涵养能力进行研究,结果表明,0-20 cm土层土壤含水量、土壤毛管孔隙度、总孔隙度、枯落物蓄积量和蓄水量均表现为:坡下>坡中>坡上,土壤含水量变化范围为278.71~377.98 g/kg,平均值为327.67 g/kg;整个坡面土壤毛管孔隙和总孔隙度平均值分别为29.08%和53.15%;枯落物蓄积量和最大蓄水量分别为16.72,53.24 t/hm2。0-20 cm土层土壤容重随坡位降低有减小趋势,其平均值为0.84 g/cm3。土壤非毛管孔隙、土壤毛管蓄水量、有效蓄水量、最大蓄水量均表现为:坡下>坡上>坡中。整个坡面平均毛管蓄水量、有效蓄水量和最大蓄水量分别为625.90,499.05,1 130.29 t/hm2。樟子松天然林林地蓄水能力也表现为:坡下>坡上>坡中,坡下为1 358.51 t/hm2,坡上为1 102.09 t/hm2,坡中为1 058.85 t/hm2,平均蓄水量为1 183.54 t/hm2。由此可见,山地樟子松天然林蓄水能力受坡度和坡位影响较大。

关 键 词:大兴安岭  樟子松天然林  坡位  土壤孔隙度  蓄水量

Research on Physical Properties of Soil Moisture and Water Conservation of Scotch Pine Forest in Da Xing'an Mountains
LI Yi,MAN Xiu-ling,CAI Ti-jiu,SHENG Hou-cai.Research on Physical Properties of Soil Moisture and Water Conservation of Scotch Pine Forest in Da Xing''an Mountains[J].Journal of Soil and Water Conservation,2011,25(2):87-91,96.
Authors:LI Yi  MAN Xiu-ling  CAI Ti-jiu  SHENG Hou-cai
Institution:LI Yi,MAN Xiu-ling,CAI Ti-jiu,SHENG Hou-cai(Northeast Forestry University,Harbin 150040)
Abstract:Physical properties of soil moisture and water conservation of scotch pine forest was studied in Da Xing'an Mountains.The results showed that,soil moisture,soil capillary porosity,total porosity,the amount of litter accumulation and water storage of 0-20 cm soil layer were as follows: lower slope>middle slope>upslope,soil moisture ranged from 278.71 g/kg to 377.98 g/kg,with an average of 327.67 g/kg;the average of soil capillary porosity and total porosity for the whole slope were 29.08% and 53.15% respecti...
Keywords:Da Hinggan Mountains  scotch pine natural forest  slope position  soil porosity  water storage  
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