کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4571297 1629231 2014 12 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Assessing channel response of a long river influenced by human disturbance
ترجمه فارسی عنوان
ارزیابی پاسخ کانال یک رودخانه طولانی تحت تأثیر اختلالات انسان است
کلمات کلیدی
تکامل مورفولوژیکی، مدل هیدرولیک رسیدن به تعریف، معدن گرانیت، میانه رود لوور
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


• Methodology to assess long-term channel changes of a long anthropogenised river
• Geomorphic and hydraulic parameters calculated on the Middle Loire River
• Application of simple statistical tests to delineate homogeneous river reaches
• Channel changes at the reach scale largely controlled by former extraction sites
• W/D and τeff/τcr, using a 1D model, yield a better understanding of the river dynamic.

This paper describes an approach to assess channel changes of a long anthropogenised river (the Middle Loire River) over decadal timescales. Channel changes are evaluated along geomorphically homogeneous river reaches. The classic geomorphic parameters (active channel width, bed slope, grain size) are complemented with parameters extracted from a 1D hydraulic model: width–depth ratio, effective bed shear stress and specific stream power calculated for the biennial discharge assimilated to bankfull flow conditions. The delineation of reaches is undertaken by combining visual inspection with the implementation of simple statistical tests to corroborate discontinuities in flow and sediment transport. The 450 km long study area has been divided into 167 homogeneous reaches. The general trends observed over the last fifty years are narrowing of the active channel width and incision of the river bed. However, changes in bed level and active channel width are not consistently correlated. Channel changes at the reach scale are mainly controlled by the presence of former sediment extraction sites. Significant incision is observed at the peak of the in-stream sediment mining period. This was followed by channel recovery when extractions stopped. The 1D numerical model provides a more rigorous manner to derive hydraulic parameters. The effective bed shear stress made dimensionless by its critical value and the width–depth ratio helps to explain observed channel responses more effectively by relating patterns to geological units along the Middle Loire.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: CATENA - Volume 121, October 2014, Pages 1–12
نویسندگان
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