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首页> 外文期刊>Soil Science Society of America Journal >Soil Carbon and Nitrogen Accumulation in a Forested Debris Flow Chronosequence, California
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Soil Carbon and Nitrogen Accumulation in a Forested Debris Flow Chronosequence, California

机译:森林泥石流时序中的土壤碳和氮积累

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摘要

The role of forest soils in the biogeochemical cycling of C and N is most dynamic during the early stages of soil development. To define C and N trends that occur with soil development in a mixed coniferous forest, a chronosequence formed by debris flows was studied. The accumulation rates of total organic C (TOC) and total N (TN) were evaluated in soils on 10 debris flow deposits, ranging from <1 to 244 yr old. Analysis of the mineral soils was restricted to the 30-cm depth, since this was the depth of the shallowest debris flows. Carbon was found to accumulate in the organic horizons at a rate of 26.5 g m–2 yr–1 throughout the time span of the chronosequence. Total organic C accumulation in the mineral horizons (0–30 cm) occurred from 0 to 82 yr at a rate of 13 g m–2 yr–1, and was nearly stable from 82 to 244 yr. Total N accumulated at a rate of 0.57 g m–2 yr–1 in the organic horizons and a rate of 0.17 g m–2 yr–1 in the mineral horizons (0–30 cm) throughout the 244 yr chronosequence. This study suggests that C accumulation in the upper mineral horizons of young forest soils occurs for 250 yr. Carbon and N accumulation in the organic horizons, however, both follow a linear trend over the 244-yr period. The rates of C accumulation suggest a rapid recovery of the soil organic C pool following disturbance.
机译:在土壤发育的早期,森林土壤在C 和N的生物地球化学循环中的作用最为动态。 定义随着土壤的发展而发生的C和N趋势。 一种针叶林混交林,研究了由碎片 流形成的时间序列。在土壤中,在<1至244岁的10个碎屑 流沉积物上,评估了土壤中总有机C (TOC)和总氮(TN)的累积速率。对 的土壤分析仅限于30 cm深度,因为 是最浅的泥石流的深度。发现碳 在整个有机层中以26.5 gm –2 yr –1 的速率积累。时间序列的时间跨度。矿物层(0–30 cm) 中总 有机碳积累发生于0至82年,速率为13 gm –2 yr –1 ,在82至244年内几乎稳定。在有机层 中,总N累积量 为0.57 gm –2 yr –1 在整个244年的时间序列中,矿层 (0–30 cm)中的0.17 gm –2 yr –1 。这项研究 建议在 年轻森林土壤的上部矿物层中积累C长达250年。有机层中的碳和N 积累,但是都遵循244年期间的 线性趋势。碳积累速率 建议在 发生扰动后土壤有机碳库快速恢复。

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  • 来源
    《Soil Science Society of America Journal》 |2009年第5期|1504-1509|共6页
  • 作者单位

    Soil and Water Sciences Program, Dep. of Environmental Sciences, Univ. of California, Riverside, CA 92521;

    Soil and Water Sciences Program, Dep. of Environmental Sciences, Univ. of California, Riverside, CA 92521;

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