林业研究(英文版)
林業研究(英文版)
임업연구(영문판)
JOURNAL OF FORESTRY RESEARCH
2009年
3期
249-253
,共5页
积累速率%分解阶段%山地森林%有机质%人工林
積纍速率%分解階段%山地森林%有機質%人工林
적루속솔%분해계단%산지삼림%유궤질%인공림
accumulation rate%decomposition stages%hill forest%organic matter%plantation forest
在孟加拉吉大港丘陵地区,调查了热带季风气候条件下的3种人工林(7年生大叶相思(Acacia auriculiformis)林、15年生大叶相思林和18年生混交林)和1种天然林的森林凋落物及其对土壤性质的作用.结果表明,总的有机质积累随人工林树龄增加而增加,但是年积累量随之降低.在同一植被类型内,不同坡位新鲜或部分分解的凋落物有机质累计量变化较大,坡底部有机质积累量最高,沿着山坡向上逐渐减少.在15年生大叶相思人工林内,土壤整合有机物积累量变化趋势与新鲜或部分分解有机质积累量变化趋势相反.在7年生和15年生的大叶相思林以及18年龄的阔叶混交人工林内,新鲜、部分分解和完全分解(含土壤整合有机质)有机质总生产速率分别是2554.31、705.79和1028.01kg.ha-1·a-1,新鲜凋落物有机质在3种林分中的生产速率分别是38.23,19.40和30.48 kg·ha-1·a-1.3种人工林和自然林内,平均新鲜凋落物的有机质积累占有机质产出总量的32.45%,部分分解凋落物占13.50%,而全分解整合土壤有机质占54.56%.森林土壤酸度随凋落物分解阶段的深入而增加.
在孟加拉吉大港丘陵地區,調查瞭熱帶季風氣候條件下的3種人工林(7年生大葉相思(Acacia auriculiformis)林、15年生大葉相思林和18年生混交林)和1種天然林的森林凋落物及其對土壤性質的作用.結果錶明,總的有機質積纍隨人工林樹齡增加而增加,但是年積纍量隨之降低.在同一植被類型內,不同坡位新鮮或部分分解的凋落物有機質纍計量變化較大,坡底部有機質積纍量最高,沿著山坡嚮上逐漸減少.在15年生大葉相思人工林內,土壤整閤有機物積纍量變化趨勢與新鮮或部分分解有機質積纍量變化趨勢相反.在7年生和15年生的大葉相思林以及18年齡的闊葉混交人工林內,新鮮、部分分解和完全分解(含土壤整閤有機質)有機質總生產速率分彆是2554.31、705.79和1028.01kg.ha-1·a-1,新鮮凋落物有機質在3種林分中的生產速率分彆是38.23,19.40和30.48 kg·ha-1·a-1.3種人工林和自然林內,平均新鮮凋落物的有機質積纍佔有機質產齣總量的32.45%,部分分解凋落物佔13.50%,而全分解整閤土壤有機質佔54.56%.森林土壤痠度隨凋落物分解階段的深入而增加.
재맹가랍길대항구릉지구,조사료열대계풍기후조건하적3충인공림(7년생대협상사(Acacia auriculiformis)림、15년생대협상사림화18년생혼교림)화1충천연림적삼림조락물급기대토양성질적작용.결과표명,총적유궤질적루수인공림수령증가이증가,단시년적루량수지강저.재동일식피류형내,불동파위신선혹부분분해적조락물유궤질루계량변화교대,파저부유궤질적루량최고,연착산파향상축점감소.재15년생대협상사인공림내,토양정합유궤물적루량변화추세여신선혹부분분해유궤질적루량변화추세상반.재7년생화15년생적대협상사림이급18년령적활협혼교인공림내,신선、부분분해화완전분해(함토양정합유궤질)유궤질총생산속솔분별시2554.31、705.79화1028.01kg.ha-1·a-1,신선조락물유궤질재3충림분중적생산속솔분별시38.23,19.40화30.48 kg·ha-1·a-1.3충인공림화자연림내,평균신선조락물적유궤질적루점유궤질산출총량적32.45%,부분분해조락물점13.50%,이전분해정합토양유궤질점54.56%.삼림토양산도수조락물분해계단적심입이증가.
Litter fall and its effect on forest soil properties at each decomposition stages were investigated in tropical monsoon climatic con-ditions of three plantations (7-year acacia plantation, 15-year acacia plantation and 18-year mixed plantation) and one natural forest (Si-tapahar forest) from Chittagong hilly region of Bangladesh. Results showed that total accumulation of organic matter increased with planta-tion age, accompanying with a decrease of annual accumulation rate. Within the same vegetation type, the organic accumulation of both fresh and partially decomposed litter with humus varied significantly (/,5_0.05) on hill positions, being highest on bottom slone and de-creased gradually towards hilltop in the forest. Reverse trend in accumulation of soil organic matters was shown in 15-year Acacia auriculi-formis plantation, from where fuel wood collected. In 7- and 15-year acacia and 18-year mixed broadleaved plantations, rates of total or-ganic matter production consisting of flesh, partially and completely decomposed litter as well as incorporated organic matter in soil were litter with humus 13.50% and incorporated organic matter in soil 54.56% of the total organic matter production with mean litter thickness of 0.90 cm. Soil acidity increased with the increase of decomposition stage of organic matter.