Field data was collected systematically to characterize the geomorphic variations in a river transition from the southern Blue Ridge to the Piedmont physiographic regions in South Carolina. Ten study reaches were surveyed for cross-sections and longitudinal profiles. Surface grid samples of bed material collected. Downstream hydraulic geometry and downstream fining of bed material were analyzed using traditional power functions and exponential decay relationships. Reach-scale channel bed morphology (bedforms) was analyzed under the assumption that the transition in bedforms is related to changes in hydraulic geometry and sediment characteristics. Well-developed downstream trends of hydraulic geometry variables (width, depth and velocity) an...
I. Project Scope | The Valley and Ridge is perhaps the case example of how rock type and structure i...
Regional curves of hydraulic geometry are frequently constructed for physiographic provinces, region...
The bed texture of a gravel-bed river is related to the size distribution and quantity of source sed...
Field data was collected systematically to characterize the geomorphic variations in a river transit...
The South Carolina Pee Dee Project (SCPDP) aims to develop a method for the determination of Minimum...
The processes involved in fluvial geomorphic adjustment to human-induced change are not well underst...
2014 S.C. Water Resources Conference - Informing Strategic Water Planning to Address Natural Resourc...
In the South Carolina Blue Ridge, Ecoregion 66, six streams were visited in April, 2019, to collect ...
Humans have had a ubiquitous influence on fluvial systems worldwide (Wohl, 2013). Landscape modifica...
Process-based approaches for river restoration are encouraged in the literature so designed rivers c...
2013 Fall.Includes bibliographical references.Many of the conceptual models developed for river netw...
Mountain rivers can be subject to strong constraints imposed by changes in gradient and grain size s...
Alluvial river channels are self-formed by the sediment-laden flow that is supplied to them from ups...
Three subhypotheses were constructed following a review of the literature and development of a theor...
Agricultural land use near streams frequently results in long-term disturbance to woody riparian veg...
I. Project Scope | The Valley and Ridge is perhaps the case example of how rock type and structure i...
Regional curves of hydraulic geometry are frequently constructed for physiographic provinces, region...
The bed texture of a gravel-bed river is related to the size distribution and quantity of source sed...
Field data was collected systematically to characterize the geomorphic variations in a river transit...
The South Carolina Pee Dee Project (SCPDP) aims to develop a method for the determination of Minimum...
The processes involved in fluvial geomorphic adjustment to human-induced change are not well underst...
2014 S.C. Water Resources Conference - Informing Strategic Water Planning to Address Natural Resourc...
In the South Carolina Blue Ridge, Ecoregion 66, six streams were visited in April, 2019, to collect ...
Humans have had a ubiquitous influence on fluvial systems worldwide (Wohl, 2013). Landscape modifica...
Process-based approaches for river restoration are encouraged in the literature so designed rivers c...
2013 Fall.Includes bibliographical references.Many of the conceptual models developed for river netw...
Mountain rivers can be subject to strong constraints imposed by changes in gradient and grain size s...
Alluvial river channels are self-formed by the sediment-laden flow that is supplied to them from ups...
Three subhypotheses were constructed following a review of the literature and development of a theor...
Agricultural land use near streams frequently results in long-term disturbance to woody riparian veg...
I. Project Scope | The Valley and Ridge is perhaps the case example of how rock type and structure i...
Regional curves of hydraulic geometry are frequently constructed for physiographic provinces, region...
The bed texture of a gravel-bed river is related to the size distribution and quantity of source sed...