贵州林业科技
貴州林業科技
귀주임업과기
GUIZHOU FORESTRY SCIENCE AND TECHNOLOGY
2011年
2期
22-25
,共4页
李海防%刘兴伟%王金叶%唐东明%李光平%王绍能
李海防%劉興偉%王金葉%唐東明%李光平%王紹能
리해방%류흥위%왕금협%당동명%리광평%왕소능
广西%猫儿山%毛竹林%水源涵养
廣西%貓兒山%毛竹林%水源涵養
엄서%묘인산%모죽림%수원함양
Guangxi%Mao' er mountain%P. heterocycla%Water conservation function
对广西猫儿山毛竹林林冠层、凋落物层及土壤层水源涵养功能进行了研究。结果表明:毛竹林地上部分生物量为59.9t/hm2,地上各部分最大持水量与生物量成正相关(P〈0.01);林冠层截留率平均值为18.9%,截留率随降雨量增大而减少(P〈0.01);毛竹林凋落物层蓄积量为11.2t/hm2,最大持水力为13.8t/hm2;土壤总孔隙度平均值为59.2%,最大持水量为1184.1t/hm2,土壤的渗透速度和渗透系数K10自上而下逐渐降低;初渗和稳渗速率平均值分别为5.7mm/min和0.4mm/min。该研究为漓江流域毛竹林水源涵养功能量化研究提供科学依据和技术支撑。
對廣西貓兒山毛竹林林冠層、凋落物層及土壤層水源涵養功能進行瞭研究。結果錶明:毛竹林地上部分生物量為59.9t/hm2,地上各部分最大持水量與生物量成正相關(P〈0.01);林冠層截留率平均值為18.9%,截留率隨降雨量增大而減少(P〈0.01);毛竹林凋落物層蓄積量為11.2t/hm2,最大持水力為13.8t/hm2;土壤總孔隙度平均值為59.2%,最大持水量為1184.1t/hm2,土壤的滲透速度和滲透繫數K10自上而下逐漸降低;初滲和穩滲速率平均值分彆為5.7mm/min和0.4mm/min。該研究為巑江流域毛竹林水源涵養功能量化研究提供科學依據和技術支撐。
대엄서묘인산모죽림림관층、조락물층급토양층수원함양공능진행료연구。결과표명:모죽임지상부분생물량위59.9t/hm2,지상각부분최대지수량여생물량성정상관(P〈0.01);림관층절류솔평균치위18.9%,절류솔수강우량증대이감소(P〈0.01);모죽림조락물층축적량위11.2t/hm2,최대지수력위13.8t/hm2;토양총공극도평균치위59.2%,최대지수량위1184.1t/hm2,토양적삼투속도화삼투계수K10자상이하축점강저;초삼화은삼속솔평균치분별위5.7mm/min화0.4mm/min。해연구위리강류역모죽림수원함양공능양화연구제공과학의거화기술지탱。
The water conservation function of Moso bamboo forest in the storey, litter and soil was studied in Mao' er mountain. The results showed that aboveground biomass of P. heterocycla was 59.9 t/hm2, and there was a positive relationship between partial biomass and the maximum water- holding capacity (P 〈 0.01 ). The mean value of rejection coefficient in the storey was 18.9%, and the canopy rejection coefficient reduced as precipitation increases (P 〈 0.01 ). The litter accumulation was 11.2 t/hm2 and the maximum water - holding capacity in the litter was 13.8 t/hm2. The mean total porosity of the studied soil was 59.2% and the maximum soil water storage was 1184.1 t/hm2. The infiltration rate and the infiltration coefficient K10 decreased with the depth of soil increasing. The mean initial and steady infiltra- tion rate showed respectively 5.7 mndmin and 0.4 mm/min,. This study provided scientific basis and technical support for quantitative research of water conservation function in Li River area