Presentation is loading. Please wait.

Presentation is loading. Please wait.

Lecture 22 Runoff (2) Event-based Hydrographs

Similar presentations

Presentation on theme: "Lecture 22 Runoff (2) Event-based Hydrographs"— Presentation transcript:

1 Lecture 22 Runoff (2) Event-based Hydrographs
Hortonian hypothesis Hewlett hypothesis

2 Event-based Hydrographs
Separating the sources of water flow affecting hydrographs in individual events is the basis for understanding the runoff processes

3 Horton Hypothsis Rainfall on the soil surface is partitioned into two components: infiltration and overland flow. The overland flow results in the quick portion of the streamflow, and water after the infiltration contributes to the delayed flow or is evaporated. The overland flow is called infiltration-excess overland flow.

4 Horton Hypothesis The infiltration capacity reduces during a rainfall event Horton hypothesis is most suitable for Areas devoid of vegetation Arid and semi-arid areas Cultivated fields In most vegetated humid regions, the Horton hypothesis may not apply. In these regions, infiltration capacity is high, thus overland flow is small. The quickflow in these cases may result from subsurface flows and ground flows.

5 Hewlett Hypothesis All rainfall at a location infiltrates to the soil until it is saturated and the water table rises to the surface level. Overland flow occurs only after the complete soil saturation. So it is called saturation overland flow

6 Hewlett Hypothesis

7 Flow in disjunct source area
These are areas where subsurface flow convergence occurs. After the convergence, the overland flow appears, or the flow is transmitted through hydrological linkages. They are caused by Slope concavities in plan Slope concavities in cross-section Areas where the soil becomes thinner than the upslope Areas of reduced hydraulic conductivity

8 Hydrological linkages
Hydrological linkages allow the rapid transmission of water from the disjunct areas to the stream channels. Forms of the linkages include Macropores Soil pipes WR, Figure 7.3

9 Role of Throughflow The maximum rate of through flow is about 5-6 m/d, so the simple calculation for rainfall to reach the stream channels from upslope areas would suggest that the throughflow can not contribute significantly to the quick flow. However, this may not be true.

10 Role of Throughflow Thatched Roof Analogy

11 Role of Throughflow “Piston displacement”: New water added at one location forces old water at lower heights to emerge. This is a mechanism that can happen instantaneous through changes in the water potential distribution in the system. Throughflow can therefore contribute to the quickflow in a very short time. This piston mechanism can only work when the soil is saturated or near saturated

12 Role of Ground Water Groundwater generally moves slowly and contribute insignificantly to storm flows, but there are many situations where groundwater flows can play an important part in storm hydrographs. These situations may include: Shallow water table, where ground water and surface water is interlinked, e.g., The Netherlands Groundwater ridge adjacent to the stream channel Conditions for the piston displacement

Download ppt "Lecture 22 Runoff (2) Event-based Hydrographs"

Similar presentations

Ads by Google