کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4533669 | 1325207 | 2007 | 10 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Critical erosion profiles in macro-tidal estuary sediments: Implications for the stability of intertidal mud and the slope of mud banks
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی
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![عکس صفحه اول مقاله: Critical erosion profiles in macro-tidal estuary sediments: Implications for the stability of intertidal mud and the slope of mud banks Critical erosion profiles in macro-tidal estuary sediments: Implications for the stability of intertidal mud and the slope of mud banks](/preview/png/4533669.png)
چکیده انگلیسی
Vertical profiles of the critical erosion threshold (Ïcrit) in sediment have been measured at 11 stations along the axis of the Tamar Estuary and at a single station in a tributary of the Tamar at St. John's Ford. The Ïcrit of surface sediment increased from 0.04 Pa in the upper, brackish estuary to 0.09 Pa in the lower estuary. In the upper estuary Ïcrit only increased slightly with depth whereas in the marine estuary Ïcrit increased rapidly from 0.09 Pa at the surface to 0.25 Pa at 15 cm below the sediment surface. The results showed that the relationship between Ïcrit and bulk density (Ïb) obtained previously for surface sediment was also applicable to sediments from depths of 10-15 cm and probably deeper. Profiles of Ïb were measured to depths of 70 cm using a corer. In the lower (marine) estuary Ïb increased with depth in the sediment from 1580 kg mâ3 at the surface to 1720 kg mâ3 at 70 cm. In the upper estuary Ïb values were lower at 1170-1200 kg mâ3 and profiles were almost homogeneous indicating that consolidation was not occurring. The mid-estuary was transitional between these two situations. These results are consistent with the seasonal accumulation and loss of 'mobile' sediment observed previously in the upper estuary with changes in river flow, and with the apparent stability of intertidal mud in the lower marine estuary deduced from historical bathymetric survey records. The slopes of the intertidal mud banks ranged from 1-2% in the lower estuary to 20-25% in mid-estuary but, instead of continuing to increase in steepness towards the head as the estuary became narrower, the measured slopes actually decreased. It is speculated that the lack of consolidation through continual mobilisation and settlement cycles combined with an increase in silt content in the upper estuary resulted in sediment that lacked the mechanical strength to maintain steep slopes.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Continental Shelf Research - Volume 27, Issue 18, 1 November 2007, Pages 2303-2312
Journal: Continental Shelf Research - Volume 27, Issue 18, 1 November 2007, Pages 2303-2312
نویسندگان
A.J. Bale, J.A. Stephens, C.B. Harris,