CHANGES IN CHANNEL PATTERN OF RIVER GANGA BETWEEN MUSTAFABAD AND RAJMAHAL, GANGETIC PLAINS SINCE 18TH CENTURY

查看全文 作　　者：Prabhata K. [1]SWAMEE;Barham [1]PARKASH;Jayaprakash V [1]THOMAS; Satvindar [1]SINGH

机构地区：[1]Emeritus Fellow, Department of Civil Engineering, Indian Institute of Technology Roorkee, Roorkee 247 667, India. Prof, Earth Sciences Dept, Indian Institute of Technology Roorkee, Roorkee 247 667,India. Formerly Postgraduate Student, Earth Sciences Dept., Indian Institute of Technology Roorkee, Roorkee 247 667,,India. Research Fellow, Earth Sciences Dept., Indian Institute of Technology Roorkee, Roorkee 247 667, India.

出　　处：《International Journal of Sediment Research》索引2003年第18卷第3期,共13页

摘　　要：Morphological analyses require quantitative description of river course by providing its equation. Such an equation is not possible as the river plan-form contains loops that cannot be described by it. To circumvent this difficulty a system of parametric equations is devised for describing the river plan-form.The system of equations was used to obtain morphological attributes like sinuosity and curvature. Using the plan-form data for the River Ganga for years 1780, 1828, 1853, 1935 and 1978 the parametric equations were setup for these years. The plan-forms were to study the changes in channel pattern,sinuosities and mode of movement of meander loops with time in the last two centuries and in the downstream direction in the Ganga River between Mustafabad and Rajmahal over about 900 km long course. 关键词：ALLUVIAL stream, Fourier series, Curvature, Meanders, Morphology, Plan-form, RIVER course, RIVER Ganga, SINUOSITY

相关文献

参考文献（11）
引证文献（3）
耦合文献（0）

参考文献(11)

引证文献(3)

互联网出版许可证新出网证(渝)字10号全国400电话 - 免长途话费

CHANGES IN CHANNEL PATTERN OF RIVER GANGA BETWEEN MUSTAFABAD AND RAJMAHAL, GANGETIC PLAINS SINCE 18TH CENTURY

参考文献(11)

引证文献(3)

用户提示