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qixianliu木虫 (小有名气)
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求助翻译摘要中的一段
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| 草丛和灌草丛两个坡地上坡位HC1、HG1和HG2剖面土壤主要是基岩风化物和植物残体堆积而成的砂质新成土，砂粒土壤含量较高，土壤中有机碳含量虽然高于下坡位各个剖面土壤，但有机碳主要贮存在砂粒土壤中，其碳库处于较不稳定状态，而下坡位剖面中土壤主要以粉粒和黏粒土壤为主，土壤有机碳含量相对较低，但主要贮存在粉粒和黏粒土壤中，其碳库处于相对稳定的状态。稀疏灌丛和乔木林两个坡地各地形剖面中主要以粉粒和黏粒土壤为主，各个剖面之间变化幅度较小，有机碳也主要贮存在粉粒和黏粒土壤中，其碳库组成比较稳定。 |
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| Both of the grass and shrub bushes bit uphill slope HC1, HG1, and HG2 soil profile is mainly made of weathered bedrock material and plant debris deposited by the new sandy soil, sand soil with a high level of soil organic carbon content while the high - various places in the downhill section of the soil, but the main organic carbon stored in the sand soil, the carbon pool in a relatively unstable, and the slope of the soil profile mainly silt and clay-based soil, soil organic carbon content relative lower, but the main stored in the silt and clay soil, the carbon pool in a relatively stable status. Lin shrubbery and trees around the two slope-shaped profile in mainly silt and clay soil mainly Change between the various profiles lesser extent, organic carbon is mainly stored in the silt and clay soil, the carbon pool relatively stable component. |
2楼2009-04-09 00:06:38
qixianliu
木虫 (小有名气)
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3楼2009-04-09 00:34:40
4楼2009-04-09 02:39:13
5楼2009-04-09 02:40:29
qixianliu
木虫 (小有名气)
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6楼2009-04-09 10:49:04
★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★
qixianliu(金币+10,VIP+0):较好 4-10 09:50
zap65535(金币+9,VIP+0):补发 12-22 02:51
qixianliu(金币+10,VIP+0):较好 4-10 09:50
zap65535(金币+9,VIP+0):补发 12-22 02:51
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Soil in the profiles HC1, HG1 and HG2 in the uphill slope area covered with brushwood, and shrub and grass belongs to sandy primosols developed on weathered bedrock and plant residues, with higher content of sand. Although organic carbon contents of these profiles were higher than those in downhill area, organic carbon was found mainly in sand, resulting in a less stable carbon pool. In soils in the downhill profiles, relatively low content of organic carbon was found in silt and clay, which are the primary components of these soils, with a relatively stable carbon pool. Soil in the profile under sparse bush and arbor woods were mainly silt and clay, regardless of their topography, slight variance of soil texture was noticed between different profiles. In soils under these two vegetations, organic carbon mainly stored in slit and clay, composition of the carbon pool is comparatively stable. 仅供参考，水平有限。 一个小建议：窃以为汉语有些不够简练。 |
7楼2009-04-10 08:06:12