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An Empirical Investigation on Hydro-Morphological Process of Surma River: Substantiation from North-East Zone of Bangladesh

机译:苏尔马河水文形态过程的实证研究:来自孟加拉东北地区的实证研究

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Objectiveof the study is to know the inherent morphological process of the river systemin the Haor areas of sylhet basin. The specific objective is to “validate theexisting conceptual Model of the CEGIS”. This research for the validation ofthe CEGIS Model. Primary data was collected through routine measurements ofdischarge, sediment concentration, measurements of cross-sections, sedimentconcentration measurements. Secondary data was collected on water level,discharge, velocity and cross-section from the BWDB. Satellite images have beencollected from USGS. A thorough review of the manuals of different numericalmodels were carried out. After evaluation of the models HEC-RAS 5.0.3 has beenselected. Validation of the CEGIS conceptual Model was tried using bothconventional way of data analysis as well as from model output. Both the modelshave been fine-tuned and simulated to predict the future scenarios with 20%increase of discharge as well as 20% decrease of discharge at the upstream.Findings of the study confirms the acceptability of Hypothesis 1, Hypothesis 2could not be (conclusively) validated. Concluded that, the bankfull waterlevels at the downstream decrease, changes in channel dimension, the change ofboth the area and the top width shows a scattered pattern and change of averagedepth shows a decreasing trend towards downstream direction. (i) Conventionalanalysis, Hypotheses 3 may be considered validated (ii) From Model output, itmay be stated that the Hypothesis 3 may be considered as not validated.Hypotheses 4 and 5 relate to the hypothetical ‘Regime Condition’ of the river.Its clear that the Surma River is not in ‘Regime Condition’. So the hypothesiscould not be validated through the model output. But ‘Regime Condition’ is atheoretical condition of a river, the validity of these two hypotheses (4 and5) can be accepted on Theoretical explanation basis.
机译:研究的目的是了解锡尔赫特河流域哈尔地区河流系统的固有形态过程。具体目标是“验证CEGIS的现有概念模型”。本研究为CEGIS模型的验证。通过常规测量流量,沉积物浓度,横截面测量值,沉积物浓度测量值收集主要数据。从BWDB收集了有关水位,流量,流速和横截面的辅助数据。卫星图像已从美国地质调查局收集。对不同数值模型的手册进行了全面回顾。在评估模型之后,选择了HEC-RAS 5.0.3。 CEGIS概念模型的验证使用常规的数据分析方法以及来自模型输出的方法进行了尝试。都对模型进行了微调和仿真,以预测未来情景,即上游排放量增加20%,而排放量减少20%。研究结果证实假设1,假设2不能被接受(最终)已验证。结论是,下游河滩水位下降,河道尺度变化,面积和顶部宽度的变化均呈分散状,平均深度的变化向下游方向减小。 (i)传统分析中,假设3可以被认为是有效的(ii)从模型输出中可以得出假设3可以被认为是未经验证的假设4和5与假设的河流``状况''有关。苏尔马河不在“地区状况”中。因此,该假设不能通过模型​​输出进行验证。但是“条件条件”是一条河流的理论条件,这两个假设(4和5)的有效性可以在理论解释的基础上接受。

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