Drainage network characteristics of the Ghaghghar River Basin (GRB), Son Valley, India

Singh, S. K.; Kanhaiya, S.; Singh, Ankita; Chaubey, K.

doi:10.1080/24749508.2018.1525670

Cited by 37 publications

(9 citation statements)

References 29 publications

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“…This study aimed to evaluate whether turbidity could produce a satisfactory estimate of TSS and little work has been done to assess the accuracy of correlating TSS to turbidity in lake urbanizing of the Tasik Kenyir, Terengganu. National water quality standard for Malaysia is a one of tool to evaluate the water quality of the Tasik Kenyir included the possible sources from anthropogenic activities which influenced the water quality were also given, many researchers have used the water quality index which involves the classification of rivers or river segments into classes of quality [6][7][8][9][10][11].…”

Section: Introductionmentioning

confidence: 99%

Potential of field turbidity measurements for computation of total suspended solid in Tasik Kenyir, Terengganu, Malaysia

Kamarudin¹,

Wahab²,

Samah³

et al. 2020

Desalination and Water Treatment

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The urbanization has significant effects on watershed hydrology and the quality of water in this catchment. One component of water quality is total suspended solids (TSS) which a significant part of physical and degradation and a good indicator of other pollutants on the surface of sediment in suspension. The purpose of this study is to investigate whether turbidity could produce a satisfactory estimate of TSS in urbanizing at the Tasik Kenyir. TSS and Turbidity were analyzed based on in-situ and ex-situ analyses were carried out according to the correlation matrix and linear regression methods at 14 (10-140 m) different depths for two sampling locations in the Tasik Kenyir (which are Chomor River and Mahadir Island-the name of sampling location in Tasik Kenyir), using data compiled. A log-linear model showed a strong positive correlation between TSS and Turbidity with is (R 2 = 0.991 for Chomor River and R 2 = 0.995 for Mahadir Island) with a regression equation of ln (TSS) = 1.32 ln (NTU) + C, with C not significantly different. From the result, water quality parameter (TSS and Turbidity) showed outlet significantly which decreased over depth caused the water quality deterioration of Tasik Kenyir development. These results strongly suggest that turbidity is a suitable monitoring parameter where water-quality conditions must be evaluated.

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Section: Introductionmentioning

confidence: 99%

Potential of field turbidity measurements for computation of total suspended solid in Tasik Kenyir, Terengganu, Malaysia

Kamarudin¹,

Wahab²,

Samah³

et al. 2020

Desalination and Water Treatment

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“…By analyzing the applicability of the four major methods, Zhong et al (2006) believes that the Hydrological Index Method is the optimal method for studying the rivers in China. Given that the studies on ecological base flow began late in China, domestic scholars have mostly adopted overseas methods during the early stage (Zhang and Xiong, 2017;Singh et al, 2019;Chacko et al, 2021). Subsequently, some domestic scholars have improved their calculation methods based on the actual circumstances of the study area.…”

Section: Introductionmentioning

confidence: 99%

Comparative study on the calculation methods of ecological base flow in a mountainous river

Gao

Hao

Song³

et al. 2022

Front. Environ. Sci.

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As the social economy is further developed, there have been increasingly severe ecological and environmental issues. For instance, rivers located in mountainous areas are often encountered with the issue of zero flow. The ecological base flow was put forward to ensure the continuous flow of rivers, to realize the minimum ecological function, and to meet the most fundamental requirements of sustaining the river ecosystem. Wulong River Basin in Yantai City of China was taken as example here. Based on the runoff data collected in the Tuanwang Hydrological Station from 1960 to 2016, the measured runoff data was restored to natural runoff sequence by adopting the item-by-item investigation method. The different ecological base flows of Wulong River were calculated by adopting the Tennant Method, the Qp90 Method, the Texas Method, the Base Flow Ratio Method, the Tessman Method, and Wetted Perimeter Method. The research findings have shown that the Base Flow Ratio Method proves to be the optimal approach for calculating the ecological base flow of Wulong River. Based on the analysis of the assurance degree of ecological base flow, the period from April to June is the period with the lowest assurance degree of ecological base flow.

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“…Morphometry is the measurement and mathematical analysis of the configuration of the earth's surface, shape, and dimensions of its landforms (Clarke, 1996). In recent years, the morphometric analysis has emerged as a powerful tool to identify and interpret the neotectonic signatures, which controls the basin dynamics of a river (Thomas, Joseph, & Thrivikramaji, 2010;Pareta & Pareta, 2011;Singh & Kanhaiya, 2015;Kaushik & Ghosh, 2015a, 2015bPrakash, Singh, & Shukla, 2016a;Prakash, Mohanty, Singh, Chaubey, & Prakash, 2016b;Prakash, Chaubey, Singh, Mohanty, & Singh, 2017a;Prakash, Mohanty, Pati, Singh, & Chaubey, 2017b;Prakash, Singh, Mohanty, Chaubey, & Singh 2017c;Rai, Chandel, Mishra, & Singh, 2018;Kanhaiya, Singh, Singh, Mittal, & Srivastava, 2018;Singh, Kanhaiya, Singh, & Chaubey, 2018a;Singh et al, 2018b). The quantitative analysis of river basin evaluation, watershed prioritization, soil and water conservation, and natural resources management at micro level has been defined using different morphometric parameters (Rudraiah, Govindaiah, & Srinivas, 2008).…”

Section: Introductionmentioning

confidence: 99%

Geomorphic evolution of the Dongar River Basin, Son Valley, Central India

Kanhaiya

Singh

et al. 2019

Geology, Ecology, and Landscapes

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The present study is an attempt to describe the geomorphic evolution of the Dongar River Basin, Son Valley, Central India. To achieve this target, a detailed field survey and morphometric analysis of the river have been carried out using Cartosat-DEM data with the help of ArcGIS 10 software. The basin area of the Dongar River is 35.17 km 2 having trellis and sub-dendritic to dendritic drainage patterns. The Dongar River is designated as fourth-order basin and lower order streams mostly dominate in the basin with the drainage density value of 1.21 km −1 . The stream order of the basin is predominantly controlled by physiographic and tectonic set-up of the study area. The slope of basin varies from 0°to 42.04°and is mainly controlled by the local geology and erosional cycles. The bifurcation ratio (Rb) for the studied basin varies from 1.58 to 4. The higher values of the bifurcation ratio, i.e., of second/third along with third/fourth order, reveal the regional geological and tectonic controls when river starts draining along the exposures of lower Vindhyan . The elongation ratio of the basin is 0.86 thus indicates high infiltration capacity, low runoff, and low-to-moderate slope of the river basin. The increase in stream length ratio from lower to higher order shows that the basin has reached mature geomorphic stage. The major trends of lineaments are ENE -WSW, i.e., almost analogous to Son-Narmada lineament suggesting that Son-Narmada lineament played an important role to control the drainage dynamics and evolution of the adjacent river basins. These features along the Dongar River and the orientation of the major lineaments suggest neotectonics, may be due to reactivation of the Son-Narmada lineament.

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Drainage network characteristics of the Ghaghghar River Basin (GRB), Son Valley, India

Cited by 37 publications

References 29 publications

Potential of field turbidity measurements for computation of total suspended solid in Tasik Kenyir, Terengganu, Malaysia

Potential of field turbidity measurements for computation of total suspended solid in Tasik Kenyir, Terengganu, Malaysia

Comparative study on the calculation methods of ecological base flow in a mountainous river

Geomorphic evolution of the Dongar River Basin, Son Valley, Central India

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