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Drainage density is a quantity used to describe physical parameters of a drainage basin. First described by Robert E. Horton, drainage density is defined as the total length of channel in a drainage basin divided by the total area, represented by the equation
Relation to water balance, Elementary components of drainage basins & Overview
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drainage density basin channel vegetation channels equation water precipitation hillslope infiltration baseflow erosion flow source average area hydrograph streams system
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Drainage density | is a | quantity used to describe physical parameters of a drainage basin | 0.90 | text |
| Drainage density | is a | function of vertical hydraulic conductivity | 0.90 | text |
| small erosive events do no develop into channels | instance of | and small perturbations | 0.80 | text |
| sheet flow or channel flow tend to incise | instance of | but rather fluvial erosive processes | 0.80 | text |
| erode to form a singular channel | instance of | but rather fluvial erosive processes | 0.80 | text |
| rain splash | instance of | which results in physical erosion processes | 0.80 | text |
| dry ravel | instance of | which results in physical erosion processes | 0.80 | text |
| or freezing | instance of | which results in physical erosion processes | 0.80 | text |
| thawing processes | instance of | which results in physical erosion processes | 0.80 | text |
| Drainage density | related to Effect of climate change on drainage density | Drainage | 0.60 | section |
| Drainage density | related to Effect of climate change on drainage density | Langbein | 0.60 | section |
| Drainage density | related to Effect of climate change on drainage density | Schumm | 0.60 | section |
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