Smakhtin and baseflow
Webb31 jan. 1995 · Abstract: Baseflow is the portion of streamflow that is sustained between precipitation events, fed to stream channels by delayed (usually subsurface) pathways. Understanding baseflow processes is critical t... read more Topics: Baseflow (76%), Watershed (53%), Streamflow (53%) View PDF 369 Citations Cite Share 1 2 3 4 5 6 … Webb15 apr. 2004 · Additionally, baseflow separation will be undertaken using the method as developed by Smakhtin, 2001. This will provide an indication as to the groundwater …
Smakhtin and baseflow
Did you know?
WebbContinuous baseflow separation from time series of daily and monthly streamflow data. Denis Hughes. 2004, Water SA. Continue Reading. Download Free PDF. Download. Related Papers. Ecological impacts of small dams on South African rivers: Part 1: Drivers of change – water quantity and quality. WebbITS OK water article lithological and tectonic control on groundwater contribution to stream discharge during conditions stefanie wirth claire carlier fabien
WebbBaseflow (sometime used as an important low-flow index) is an important genetic component of streamflow, which comes from groundwater storage or other delayed … WebbBaseflow-controlling pro-cesses in polar and arid settings are sufficiently unique to merit specific treatment elsewhere. The introductory section covers a basic defini-tion of baseflow, as well as discussion of pri-mary controls on baseflow and various approaches to quantification. Next, a section on geomorphic controls on baseflow discharge
WebbThis paper describes a parsimonious approach for the evaluation of wetland hydrological functions, based on continuous observed streamflow records and flow duration curves. … Webbbaseflow correlation Christine F. Reilly1 and Charles N. Kroll ... [Smakhtin, 2001]. In the United States, the 7-day, 10-year low flow (Q 7,10) is a commonly used low-flow statistic [Riggs, 1980]. The Q 7,10 is the average annual 7-day minimum flow that is …
Webb21 aug. 2012 · The reviews of Hall, 1968, Smakhtin, 2001 and Schwartz (2007) provide a history of methods for baseflow separation, and discuss the problems related to the definition of baseflow, as well as the underlying assumptions of …
Webb3 dec. 2024 · The understanding of hydrogeological characteristics and groundwater flow processes in aquifers is crucial for the determination of sustainable groundwater resource development as well as hydrological management and planning. In the past, information on hydrogeological characteristics was mainly acquired through point field measurement … grapetree travel assignmentsWebb1 okt. 2024 · The objectives of this study are to: 1) present a new modelling framework to simulate base flow from a subsurface model using both groundwater and streamflow … chip reese bioWebbKeywords: Baseflow separation, rainfall, streamflow, continuing loss, design floods, loss estimates. ABSTRACT Rainfall runoff models are used to estimate design ... (1990) and Smakhtin (2001) separated the flow components on the basis of travel times. The “old flow” is identified as being water that was already in the catchment before the chip reeves bankingWebb5 okt. 2024 · As Price (2011) has noted, there are four broad approaches to quantify baseflow, as follows: low-flow event time series, flow-duration statistics, baseflow … grape tree texasWebbFor example, reductions in baseflow dis-charges affected fish species richness and density more severely in smaller (low-order) than in larger (higher-order) streams in Georgia, USA (McCargo and Peterson ... (Smakhtin 2001). These factors, in turn, influence aquatic and terrestrial ecosystems by altering the mechanistic relationships chip reese net worthWebb15 apr. 2004 · V. Smakhtin Published 15 April 2004 Environmental Science Water SA The paper describes a simple technique for baseflow separation from continuous monthly … chip reese wikiWebb13 feb. 2010 · Results have showed that: baseflow recession constant in Wudinghe River Basin ranges from 0.72 to 0.94 with a larger recession rate in flood season than that in non-flood season. Spatially, the recession rate of baseflow in loess area is the biggest, but is the smallest in the sandy area. chip reeves midwestone