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基于模擬降雨的北京褐土坡地土壤團粒流失特征試驗
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國家林業(yè)局林業(yè)公益性項目(201404209)和國家自然科學基金項目(41271300、30900866)


Particle Characteristics of Eroded Cinnamon Soil from Beijing Based on Simulated Rainfall
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    摘要:

    選取20°北京典型褐土坡面徑流小區(qū)為試驗對象,基于野外人工模擬降雨試驗和有無雨滴打擊作用對坡面侵蝕的影響,研究了坡面土壤團粒組成及其變化特征,揭示了坡面侵蝕過程中泥沙團粒的分離和輸移規(guī)律。試驗處理包括3種代表性降雨強度(35、65、100mm/h)和3種植被蓋度(0%、30%、80%)。結(jié)果表明,消除雨滴打擊作用后,坡面侵蝕特征變化明顯,坡面含沙量和土壤分離率分別減少25.91%~31.15%和35.10%~41.20%,坡面侵蝕泥沙團粒中值粒徑均小于雨滴擊濺坡面。通過侵蝕泥沙有效粒徑分布和最終粒徑分布的比值(E/U)分析泥沙團粒的粒徑分選特征,發(fā)現(xiàn)產(chǎn)流初始階段粗砂、細砂、細粉粒和粘粒多以團聚體形式存在,而粗粉砂以初級粒子形式存在;隨著降雨歷時延長,侵蝕泥沙各粒級的分離程度增加,泥沙顆粒逐步分解為初級粒子。坡面侵蝕泥沙分離規(guī)律表明,泥沙團粒結(jié)構(gòu)變化與坡面水動力學特征密切相關,土壤團聚體分形維數(shù)(D)與時間(T)呈冪函數(shù)關系。坡面產(chǎn)流前雨滴擊濺對土壤分離有重要作用,其對土壤分離貢獻率為28.09%,而無雨滴打擊坡面土壤團聚體分形維數(shù)增量是有雨滴打擊增量的48.43%。在該區(qū)坡地泥沙顆粒輸移過程中,穩(wěn)定性較差的砂粒被分解為細小顆粒,粗粉砂多以初級粒子形式存在,對坡面侵蝕泥沙顆粒分離過程具有重要影響,而粘粒在侵蝕坡面則逐漸富集。

    Abstract:

    In order to study and illuminate the effects of different raindrops and runoff characteristics on size-selectivity of sediments crumb structure detachment and transportation in soil erosion process, a rainfall simulation study was conducted to examine the sediment particle dynamic distribution characteristics in Beijing, China. Erosion plots (5m×1m) were installed in a 20° hillslope. Experiment treatments included three rainfall intensities (35mm/h, 65mm/h and 100mm/h) of representative rainfalls and three average vegetation coverages (0%, 30% and 80%). The changes of sediment crumb structure at erosion plots with and without raindrop impact were observed through placing the nylon net over the soil surface. The results showed that sediment concentration and soil loss were reduced by 25.91%~31.15% and 35.10%~41.20%, respectively, after eliminating raindrop impact. The sediment mean particle size (D50) of the slope without raindrops was less than that of the slope with raindrops, which was decreased by 23.47%, 27.17% and 31.63% under the three kinds of rainfall intensities. At the initial stage of runoff, coarse sand-size, fine sand-size, fine silt-size and clay-size existed in the form of aggregation, and coarse silt-size was in a state of primary particles. With the extension of rainfall, the E/U (effective-ultimate size) ratio of each graded size was gradually tended to be the value of 1, which indicated sediment particles existed in the form of primary particles. The correlation analysis of the sediment particle size and water flow power under different vegetation coverages showed that the slope erosion process was closely related to the hydrodynamic characteristics. The effect of splash on soil surface accounted for 28.09% of the total detachment degree before the runoff generation, and the soil aggregate fractal dimension increment with no raindrops on the slope was 48.43% of that with raindrops on the slope. In the sediment transport process, sand particles was decomposed into small particles, coarse silt particles were transported as primary particles, and clay particles was gradually enriched in the erosion process. The sediment size-selectivity characteristics by erosion dynamics in the process of erosion were revealed, which deepened the research on erosion regularity of different erosion processes.

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楊帆,張洪江,程金花,周柱棟.基于模擬降雨的北京褐土坡地土壤團粒流失特征試驗[J].農(nóng)業(yè)機械學報,2016,47(8):137-145,215. Yang Fan, Zhang Hongjiang, Cheng Jinhua, Zhou Zhudong. Particle Characteristics of Eroded Cinnamon Soil from Beijing Based on Simulated Rainfall[J]. Transactions of the Chinese Society for Agricultural Machinery,2016,47(8):137-145,215.

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  • 收稿日期:2016-01-14
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  • 在線發(fā)布日期: 2016-08-10
  • 出版日期: 2016-08-10