Stem flow chemistry of Picea glehnii,Abies sachalinensis and Alnus japonica and its effect on the peat pore water chemistry in an ombrogenous mire in Ochiishi,eastern Hokkaido,Japan  

日本北海道东部高位泥沼远东红皮云杉、库页冷杉和日本桤木树干茎流化学及其对沼泽孔隙水化学的影响(英文)

作　　者：Tsutomu Iyobe Akira Haraguchi 

机构地区：[1]Research Center for Natural Hazards & Disaster Recovery,Niigata University [2]Faculty of Environmental Engineering,The University of Kitakyushu

出　　处：《Journal of Forestry Research》2010年第2期119-128,I0003,共11页林业研究（英文版）

基　　金：funded by the Grant in Aidfrom JSPS

摘　　要：We investigated the chemical properties of stemflow of Picea glehnii,Abies sachalinensis and Alnus japonica as well as peat pore water chemistry,including the distance and depth profiles of pore water chemistry,in an ombrogenous mire.The effect of stemflow on the peat pore water chemistry was clear at the stem base in the peat forest in the mire,and the peat pore water around the stem base of a tree had its own chemical properties specific to each species.P.glehnii showed the highest concentration of salts both in stemflow and peat-pore water,whereas A.japonica showed the lowest concentrations;however,the gradient of the chemical environment from the stem base to outside of the canopy is formed.The peat pore water chemistry under the canopy was mainly controlled by the chemical processes diluted by the abundant peat pore water;the stemflow movement in the high water content of the peat was more slowly because of the flat topography（〈 1o）.This would be due to the fact that the chemicals in stemflow would be diluted by the abundant peat pore water.The spatial heterogeneity of chemical environment between microsites within forested peatland would be also contributed indirectly through the control of microorganism activity,and nutrient regeneration mediated the surface water and the stemflow of the dominant canopy trees.在日本北海道高位泥沼池,调查了远东红皮云杉(Piceaglehnii)、库页冷杉(Abies sachalinensis)和日本桤木(Alnusjaponica)树干茎流液的化学性质和泥炭孔隙水的化学性质,包括了横切和纵切面孔隙水化学性质。沼泽森林树干基部茎流对泥炭孔隙水化学性质有明显的作用,而且树基部的泥炭孔隙水化学性质具有物种特异性。远东红皮云杉茎流液和泥炭孔隙水中盐分含量最高,日本桤木则最低;盐分从茎基部向树冠形成浓度梯度。树冠下泥炭孔隙水化学受化学过程控制,孔隙水充沛条件下,控制作用减弱,因地势平缓(<1°)茎流移动缓慢。事实上,泥炭孔隙水充足会使茎流化学物质浓度降低。微生物活动、优势树冠的营养再生介导的表面水和茎流对森林沼泽地微生境化学环境的空间异质性有贡献。图2表2参44。

关 键 词：Abies sachalinensis Alnus japonica Picea glehnii peat pore water STEMFLOW chemical properties 

分 类 号：S715.7[农业科学—林学]