Characteristics of decomposition of dissolved organic carbon by microbes in water of forest ecosystems

森林生态系统水中微生物分解溶解有机碳的特征

基本信息

项目摘要

A flow-through bioreactor method is useful for measurement of biodegradable dissolved organic carbon(BDOC) in water of forest ecosystems. We determined the condition of BDOC measurement as follows ; over 20℃ for air temperature, 0.25 ml/min for solution flow rate and 10 mg/L for DOC concentration of samples. The percentages of BDOC on DOC(BDOC%) in percolated water of organic layer were 20-30% in Japanese cedar (Cryptomeria japonica), Japanese cypress (Chamecyparis obutsa) and red pine (Pinus densiflora) stand, while 50% in mizunara (Quercus mongolica var.grosseserrata) stand. This result suggested that the large amount of nitrogen influenced the BDOC% in mizunara stand.In a small watershed of aged Japanese cedar and cypress plantation, DOC in order of high concentrations were organic layer percolation > through fall > precipitation, and was rapidly low in soil water. The DOC annual discharge in steam water was small (6.4 kg/ha), suggesting the DOC in soil water was consumed by soil microbes and adsorbed on soil colloid. The amount of consumption of water soluble organic carbon (WSOC) had positive correlations with the rate of carbon mineralization in surface soil. Therefore, DOC and WSOC amounts were important indicators for microbe activities. However, these amounts were remarkably smaller than mineralized carbon, so we considered that determination of available organic carbon was necessary.The percentages of lignin on humus increased with increases of decomposition class in forest floor of six species. Especially, the organic carbon in the humus class insoluble by alkaline solution had 70% of carbon in lignin. On the other hand, the amounts of lignin decreased with decreases of mass weight due to decomposition of the leaf litter of six deciduous broad-leaved trees species. We need to make more detailed classification of organic matter, such as easily or hard decomposed lignin.
流式生物反应器法是测定森林生态系统水体中生物可降解溶解有机碳(BDOC)的有效方法。我们确定BDOC测量条件如下:空气温度≥20℃,溶液流速≥0.25 ml/min,样品DOC浓度≥10 mg/L。杉木(Cryptomeria japonica)、日本柏木(Chamecyparis obutsa)和红松(Pinus densiflora)林分有机层渗透水中BDOC对DOC的百分比(BDOC%)为20 ~ 30%,水原(Quercus mongolica var.grosseserrata)林分为50%。结果表明,大量施氮对水原林分BDOC%有影响。在一个小流域的老杉柏人工林中,DOC的浓度从高到低依次为有机层渗漏>到秋季降水>,在土壤水分中迅速降低。蒸汽水中DOC年排放量较小(6.4 kg/ha),说明土壤水中DOC被土壤微生物消耗并吸附在土壤胶体上。表层土壤水溶性有机碳耗量与碳矿化率呈显著正相关。因此,DOC和WSOC量是微生物活性的重要指标。然而,这些数量明显小于矿化碳,因此我们认为有效有机碳的测定是必要的。6种植物的腐殖土中木质素含量随分解等级的增加而增加。特别是不溶于碱性溶液的腐殖质类有机碳占木质素碳的70%。另一方面,6种落叶阔叶树凋落叶的分解导致木质素含量随质量重量的减少而减少。我们需要对有机物进行更详细的分类,比如易分解和难分解的木质素。

项目成果

期刊论文数量(24)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
陸上生態系の物質循環からみた窒素飽和による汚染の構図
从陆地生态系统物质循环角度分析氮饱和污染的构成
  • DOI:
  • 发表时间:
    2002
  • 期刊:
  • 影响因子:
    0
  • 作者:
    戸田浩人
  • 通讯作者:
    戸田浩人
小柳信宏, 千原麻由, 生原喜久雄, 戸田浩人: "分解程度の異なる樹種別リターの炭素および窒素無機化特性"日本土壌肥料学雑誌. 73・4. 363-373 (2002)
Nobuhiro Koyanagi、Mayu Chihara、Kikuo Ikuhara、Hiroto Toda:“不同分解程度的树木凋落物的碳和氮矿化特征”日本土壤与肥料杂志73・4(2002)。
  • DOI:
  • 发表时间:
  • 期刊:
  • 影响因子:
    0
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  • 通讯作者:
Nitrogen and carbon mineralization characteristics of different decomposition stages in forest floor of some species.
部分树种林地不同分解阶段氮碳矿化特征
Characteristics of carbon and nitrogen dynamics in a small watershed of aged Japanese cedar and cypress stands in the northern Kanto region, Japan.
日本关东地区北部老杉和柏树小流域的碳氮动态特征。
Outline of nitrogen pollution by nitrogen saturation in nutrient circulation of terrestrial ecosystems
陆地生态系统养分循环中氮饱和造成的氮污染概述
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TODA Hiroto其他文献

TODA Hiroto的其他文献

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{{ truncateString('TODA Hiroto', 18)}}的其他基金

Forest ecosystem cycle analysis of radionuclide in organic and mineral soil
有机矿质土壤中放射性核素的森林生态系统循环分析
  • 批准号:
    24380076
  • 财政年份:
    2012
  • 资助金额:
    $ 2.24万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
Rule of organic phosphorous and microbial on phosphorous supply for vegetation in forest soil
森林土壤有机磷和微生物对植被供磷的规律
  • 批准号:
    17580125
  • 财政年份:
    2005
  • 资助金额:
    $ 2.24万
  • 项目类别:
    Grant-in-Aid for Scientific Research (C)

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