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Journal ArticleDOI

A Theoretical Analysis of Groundwater Flow in Small Drainage Basins

József Tóth
- 15 Aug 1963 - 
- Vol. 68, Iss: 16, pp 4795-4812
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TLDR
In this paper, three types of flow systems may occur in a small basin: local, intermediate, and regional, and the higher the topographic relief, the greater the importance of the local systems.
Abstract
Theoretically, three types of flow systems may occur in a small basin: local, intermediate, and regional. The local systems are separated by subvertical boundaries, and the systems of different order are separated by subhorizontal boundaries. The higher the topographic relief, the greater is the importance of the local systems. The flow lines of large unconfined flow systems do not cross major topographic features. Stagnant bodies of groundwater occur at points where flow systems meet or branch. Recharge and discharge areas alternate; thus only part of the basin will contribute to the baseflow of its main stream. Motion of groundwater is sluggish or nil under extended flat areas, with little chance of the water being freshened. Water level fluctuations decrease with depth, and only a small percentage of the total volume of the groundwater in the basin participates in the hydrologic cycle.

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Citations
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Interactions between groundwater and surface water: the state of the science

TL;DR: In this article, the mechanisms of interactions between groundwater and surface water (GW-SW) as they affect recharge-discharge processes are comprehensively outlined, and the ecological significance and the human impacts of such interactions are emphasized.
Journal ArticleDOI

Choosing appropriate techniques for quantifying groundwater recharge

TL;DR: The reliability of recharge estimates using different tech- niques is variable as mentioned in this paper, and uncertainties in each approach to estimating recharge underscore the need for application of multiple techniques to increase the expected recharge rates at a site.
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Formation and Diagenesis of Weathering Profiles

TL;DR: In this paper, the predicted bulk compositional changes are corroborated by studies of recent weathering profiles developed on a variety of plutonic and volcanic rocks under different climatic regimes.
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A comprehensive surface-groundwater flow model

TL;DR: In this article, a simple groundwater flow and height model was added to an existing basin-scale surface water model and validated on a 471 km2 watershed near Waco, Texas.
References
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Journal ArticleDOI

A theory of groundwater motion in small drainage basins in central Alberta, Canada

TL;DR: In this paper, a cross-sectional distribution of the fluid potential in a basin of homogeneous lithology is found, and a boundary between areas of recharge and discharge is proved mathematically.
Journal ArticleDOI

Laws of the formation of minimum stream flow

TL;DR: In this paper, the authors present the Law of the Minimum Stream Flow (MLW) and the International Association of Scientific Hydrology (IAHSH) for the first time.