首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >PhytOC stock in forest litter in subtropical forests: Effects of parent material and forest type
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PhytOC stock in forest litter in subtropical forests: Effects of parent material and forest type

机译:亚热带森林凋落物中的PhytOC储量:母体材料和森林类型的影响

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Organic carbon (C) occluded in phytolith (PhytOC) is stable in the soil for millennia and can be an important contributor to long-term C storage in forest ecosystems. In order to understand the effect of parent material and vegetation type on the production of PhytOC in plant litter in subtropical forests in China, we investigated the PhytOC concentration and stock in plant litter in four forest types, moso bamboo (Phyllostachys edulis Moso), Chinese-fir (Cunninghamia lanceolata), evergreen broadleaf and mixed conifer-broadleaf forests, established on three parent materials (rhyolite, sandy shale and tuff). This study showed that: 1) both parent material and forest type significantly affected phytolith concentrations in litter, and there was a significant interaction between parent material and forest type. Plant litter in the moso bamboo forest developed on rhyolite and tuff had the highest phytolith concentrations followed by moso bamboo forest on sandy shale; 2) forest type but not parent material affected PhytOC concentrations in litter, with the highest in the moso bamboo forest; 3) both parent material and forest type significantly affected PhytOC stock in litter, without a significant interaction between the two factors. The moso bamboo forest had the highest PhytOC stock in its litter; and 4) the PhytOC stock returned to the soil in moso bamboo, Chinese-fir, evergreen broad-leaf and mixed coniferous forests was (mean + SD) 14.66 + 4.69, 2.87 + 2.19, 6.22 + 2.46 and 4.84 + 1.82 kg ha(-1), respectively. Considering the area of the four respective forest types, the amount of C that can be entered into the soil in the form of PhytOC in litter was 2.08 x 10(5),1.19 x 10(5), 5.68 x 10(5) and 2.75 x 10(4) t CO2-e, respectively, and therefore it indicates a great potential in long-term C storage. (C) 2016 Elsevier B.V. All rights reserved.
机译:植硅体(PhytOC)中所含的有机碳(ChytOC)在土壤中稳定了数千年,并且可能是森林生态系统中长期C储存的重要贡献者。为了了解母本和植被类型对中国亚热带森林植物凋落物中PhytOC产量的影响,我们调查了四种森林类型(毛竹(Phyllostachys edulis Moso))中植物凋落物的PhytOC浓度和种群。杉木(Cunninghamia lanceolata),常绿阔叶和针叶阔叶混交林,建立在三种母体材料(流纹岩,砂质页岩和凝灰岩)上。这项研究表明:1)母本和森林类型均显着影响凋落物中的植硅体浓度,并且母本和森林类型之间存在显着的相互作用。在流纹岩和凝灰岩上发育的毛竹林中,植物凋落物的植酸盐含量最高,其次是沙质页岩的毛竹林。 2)森林类型而不是母本材料影响凋落物中PhytOC的浓度,在毛竹林中最高。 3)母本材料和森林类型均显着影响凋落物中的PhytOC存量,而两个因素之间没有显着的相互作用。毛竹林中的PhytOC存量最高。 4)毛竹,杉木,常绿阔叶和针叶混交林中的PhytOC储量返回土壤为(平均值+标准差)14.66 + 4.69、2.87 + 2.19、6.22 + 2.46和4.84 + 1.82 kg ha( -1)。考虑到四种森林类型的面积,以枯草中的PhytOC形式进入土壤的碳量分别为2.08 x 10(5),1.19 x 10(5),5.68 x 10(5)和二氧化碳当量分别为2.75 x 10(4)t CO2-e,因此表明其在长期C存储中具有巨大潜力。 (C)2016 Elsevier B.V.保留所有权利。

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