کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4549069 | 1627340 | 2009 | 13 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Sediment physical properties of the DYNAS study area
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
اقیانوس شناسی
پیش نمایش صفحه اول مقاله
چکیده انگلیسی
Physical properties of the deposits in the DYNAS study area, the Mecklenburg Bay, were investigated using sediment echosounders and laboratory analysis were carried out on undisturbed short sediment cores. Wet bulk densities of about 1.2Â g/cm3 for mud and up to 1.9Â g/cm3 for silty sand were found in surface sediments of the Mecklenburg Bay. Sediment density-depth functions were approximated by logarithmic regression functions at different depth intervals. Sediment consolidation was studied by both (i) consolidation tests of sediment samples and (ii) from the void ratio-overburden pressure relation in natural sediments. Low shear strength values of 9-71Â Pa were measured at the mud surface. Downcore, a depth gradient of about 14.5Â Pa/cm was calculated. Sediments with high silt and sand contents are characterized by shear strength values of up to 3000Â Pa. Published formulas derived from erosion studies were used to calculate the critical shear stress using wet bulk density and shear strength. The obtained results demonstrate clearly, that there is still a wide gap in knowledge about the relationships between erosion parameters and sediment physical properties.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Marine Systems - Volume 75, Issues 3â4, 10 February 2009, Pages 317-329
Journal: Journal of Marine Systems - Volume 75, Issues 3â4, 10 February 2009, Pages 317-329
نویسندگان
Rudolf Endler,