东北林业大学学报
東北林業大學學報
동북임업대학학보
JOURNAL OF NORTHEAST FORESTRY UNIVERSITY
2014年
10期
16-19
,共4页
王新星%赵国平%史社强%丁国栋%赵媛媛%邓继峰%高广磊
王新星%趙國平%史社彊%丁國棟%趙媛媛%鄧繼峰%高廣磊
왕신성%조국평%사사강%정국동%조원원%산계봉%고엄뢰
樟子松%细根%分布特征%陕西榆林
樟子鬆%細根%分佈特徵%陝西榆林
장자송%세근%분포특정%협서유림
Pinus sylvestrisvar .mongolica%Fine roots%Distribution characteristics%Yulin City,Shaanxi Province
采用根钻取样法对陕西榆林樟子松细根分布特征进行研究。结果表明:樟子松细根根质量密度随着距树干基部距离的增大而减小,细根集中分布在0~150 cm内,超过细根总生物量的50%。细根生物量在南北东西方向上都有差异,南方最少,北方最多,东西相差不大。在垂直方向上,细根根质量密度在0~10 cm的土层中很小,10~120 cm的土层中随着土壤深度的增加而减小,在10~40 cm的土层中细根生物量超过总细根生物量45%。土壤含水率随着土壤深度的增加先增大后减小,在10~70 cm的土层中与细根根质量密度的变化趋势相反。
採用根鑽取樣法對陝西榆林樟子鬆細根分佈特徵進行研究。結果錶明:樟子鬆細根根質量密度隨著距樹榦基部距離的增大而減小,細根集中分佈在0~150 cm內,超過細根總生物量的50%。細根生物量在南北東西方嚮上都有差異,南方最少,北方最多,東西相差不大。在垂直方嚮上,細根根質量密度在0~10 cm的土層中很小,10~120 cm的土層中隨著土壤深度的增加而減小,在10~40 cm的土層中細根生物量超過總細根生物量45%。土壤含水率隨著土壤深度的增加先增大後減小,在10~70 cm的土層中與細根根質量密度的變化趨勢相反。
채용근찬취양법대협서유림장자송세근분포특정진행연구。결과표명:장자송세근근질량밀도수착거수간기부거리적증대이감소,세근집중분포재0~150 cm내,초과세근총생물량적50%。세근생물량재남북동서방향상도유차이,남방최소,북방최다,동서상차불대。재수직방향상,세근근질량밀도재0~10 cm적토층중흔소,10~120 cm적토층중수착토양심도적증가이감소,재10~40 cm적토층중세근생물량초과총세근생물량45%。토양함수솔수착토양심도적증가선증대후감소,재10~70 cm적토층중여세근근질량밀도적변화추세상반。
By the drilling sampling , we studied the distribution of Pinus sylvestris var.mongolica fine roots in Ynlin City , Shaanxi Province .Pinus sylvse tris var.mongolica fine roots weight density decreased with the increasing distance from the base of the trunk , fine roots were mainly concentrated in the range of 0-150 cm, and exceeded 50%of the total fine root biomass.The distribution of fine root biomass were not even under four directions , least at the south, most at the north, and there was no much difference between east and west .In the vertical direction ,the fine roots weight density was less in 0-10 cm of the soil layer , decreased with the depth increasing under the 10-120 cm of the soil layer , and the fine root bio-mass exceeded 45%of the total amount in the 10-40 cm of the soil layer .The trend of soil moisture first increased and then decreased with the soil depth increasing , which showed the opposite trend in the 10-70 cm of the soil layer .