کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
5769862 1629197 2017 9 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Soil aggregate breakdown in response to wetting rate during the inter-rill and rill stages of erosion in a contour ridge system
ترجمه فارسی عنوان
تجزیه خاک در واکنش به میزان خیس شدن در طی مراحل بین فرسایش و ریل در فرسایش سیستم
کلمات کلیدی
فروپاشی کامل توزیع اندازه جامع، فرسایش بین برف، فرسایش سرخ، شبیه سازی بارش،
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


- This study was conducted in a contour ridge system.
- At the micro-aggregate scale, 20-50 and 50-100 μm fractions experienced the greatest loss.
- The collapse degree of 2-5 mm fraction was the most drastic at the inter-rill stage.
- Breakdown of 0.25-0.5 mm, 0.5-1 mm, 100-200 μm fractions was quite serious at the rill stage.
- The critical wetting rate thresholds for these seriously broken fractions was supplied.

Wetting rate is one of the major factors determining the magnitude of slaking force in soils. Differences in wetting rate result in varying degrees of soil aggregate breakdown that alters the distribution of particle sizes in sediment. The objective of the present study was to determine how various wetting rates affected soil aggregate breakdown and soil fraction distribution in a contour ridge system. In the simulated rainfall experiment, the breakdown of 16 sizes soil aggregate was evaluated under five wetting rates (10, 20, 30, 60, and 90 mm h− 1) at different stages of erosion. The greatest fraction of sediment was microaggregate (accounting for 63.66%-69.19% of the total), and 20-50 μm and 50-100 μm classes were dominant within microaggregate fraction. The obviously increased loss of sediment from these two sizes occurred mainly as a result of the breakdown of 2-5 mm and 1-2 mm fractions during the inter-rill stage of erosion, and it was induced by the collapse of 0.25-0.5 mm, 0.5-1 mm, and 100-200 μm aggregates during rill erosion. Critical wetting rate thresholds of 20 mm h− 1 controlled the breakdown of 2-5 mm and 1-2 mm fractions during the inter-rill stage. During the rill stage, when the wetting rate exceeded 10 mm h− 1, the breakdown of 0.25-0.5 mm and 0.5-1 mm sizes intensified and the critical threshold for the collapse of 100-200 μm aggregate was 20 mm h− 1. These findings enhance our understanding of the breakdown mechanism of soil aggregates and supply guidance for implementing contour ridge systems.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: CATENA - Volume 157, October 2017, Pages 241-249
نویسندگان
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