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机构地区:[1]中国林科院亚热带林业研究所,浙江富阳311400
出 处:《竹子研究汇刊》1998年第2期59-64,共6页Journal of Bamboo Research
基 金:加拿大国际发展研究中心(IDRC)的资助
摘 要:在我国毛竹主要产区浙江省安吉县灵峰寺林场试验林的三个区组中,根据立竹直径分布规律确定样竹处理数后,随机布置总共30套秆流收集装置,持续观察21个月,共获91次秆流水。测定每次秆流水量并分析其N、P、K、Ca、Mg含量以研究毛竹林内秆流的变化动态及其养分输入。结果表明:秆流水中不含Ca,其它四元素的年输入量分别为N-1.8557,P-0.0072,K-0.7849,Mg-0.1569,Kg.ha-1;年秆流量为年降水量的12.5%,无论次、月秆流量与相应降水量均为紧密线性相关,但与立竹粗度为显著非线性相关;其它因子,如:立竹所处的坡位、坡向,竹林密度,钩梢强度,立竹分布状况,植株个体表面结构特征等,亦直接或间接地影响着竹秆流的产生和大小。Based on standing bamboo diameter distribution, 30 sets of collectors for bamboo stem run-off were set up at rand0m for 21-month-long on-the-spot oberservation at threetrial blocks located in Linfengsi forest farm,Anji County,Zhejiang Province which is one ofvital moso production areas in China, targeting at finding out bamboo step run-of dynamicand nutrient element input in moso stand by measuring their stem run-off and contents of N,P,K,Ca,Mg each time.The results showed: in the run-off,no Ca element,the content of N,P,K,Mg is 1. 8557, 0. 0072, 0. 7849, 0- l569 Kg/ha respectively ;annual bamboo stem run-0ffis l2. 5% of the annual rainfall;bamboo stem run-off of each time,and month has a close lin-ear relationship with corresponding annual rainfall,but a marked non-linear relationship with standing bamboo density, meanwhile, other factors haves also direct or indirect effects on bamboo step run-off, e. g. slope site/directi0n, standing bamboo density, tipping tensity,standing bamboo distribution,surface structure features of individual bamboo,etc.
分 类 号:S795.720.1[农业科学—林木遗传育种]
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