2014
DOI: 10.1061/(asce)he.1943-5584.0000873
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Hydrologic Characterization of Undrained Porous Pavements

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Cited by 17 publications
(12 citation statements)
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“…However, evaporative losses over longer timescales are substantial, with annual values reaching 150 mm, easily 10–20% or more of an annual water budget in North America or Europe (Figure ; Göbel et al, ; Hein, Strecker, Poresky, Roseen, & Venner, ). Martin and Kaye () indicate that ~1 mm/day is a conservative ET estimate for porous pavements without underdrains. Göbel et al () estimate cold‐weather ET rates from porous pavement during December through February around 0.24 mm/day.…”
Section: Resultsmentioning
confidence: 99%
“…However, evaporative losses over longer timescales are substantial, with annual values reaching 150 mm, easily 10–20% or more of an annual water budget in North America or Europe (Figure ; Göbel et al, ; Hein, Strecker, Poresky, Roseen, & Venner, ). Martin and Kaye () indicate that ~1 mm/day is a conservative ET estimate for porous pavements without underdrains. Göbel et al () estimate cold‐weather ET rates from porous pavement during December through February around 0.24 mm/day.…”
Section: Resultsmentioning
confidence: 99%
“…Therefore, it can be assumed that stormwater can infiltrate into a PPS and reach the bottom almost instantaneously when the PPS is not filled. Thus, a PPS is usually modelled as a storage space underlined with permeable soils (Martin & Kaye, ; Schwartz, ; Zhang & Guo, ). For a PPS without underdrains, the storage spaces consist of the void portions of the pavement and storage layers; and the total storage capacity ( S m , expressed as depth of water over the surface area of the pavement) can be calculated as Sm=Sd+italicVRitalicpavement1+VRpavementDepthpavement+italicVRitalicstorage1+VRstorageDepthstorage, where S d is the surface depression storage of the pavement layer, expressed in mm of water over the surface area of the pavement; VR pavement and VR storage (dimensionless) are the void ratios of the pavement and storage layers, respectively; Depth pavement is the depth (in mm) of the pavement layer; and Depth storage is the depth (in mm) of the storage layer of the PPS.…”
Section: Event‐based Analytical Probabilistic Approach For Estimatingmentioning
confidence: 99%
“…Currently, only bottom infiltration with a constant rate is considered in the design of PPSs (e.g., in Pennsylvania, USA, PDEP, ). Therefore, in this paper, the rate of infiltration into the native soils through the bottom during a rainfall event is assumed to be constant, equalling the saturated hydraulic conductivity of the native soils (denoted as f c in mm/hr; Martin & Kaye, ; Schwartz, ). The total volume infiltrated during a rainfall event can therefore be calculated as F=fcu, where u is the duration of the event.…”
Section: Event‐based Analytical Probabilistic Approach For Estimatingmentioning
confidence: 99%
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