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- W228141463 abstract "Long-term acceptance rates (LTAR) are used in specifying the area of the bottom of drain- field trenches required for onsite wastewater systems (OWSs). Our objective is to present a simple method for converting soil saturated hydraulic conductivity (K(s)) to LTAR, given a number of assumptions about soil and biomat hydraulic properties. In this paper, we describe an Excel spreadsheet that uses a modified equation from Bouma (1975) to calculate the steady trench bottom flux in an OWS based on an input of soil K(s). The soil water retention parameters are also required, but they can be taken from a table in the spreadsheet that provides parameters for the 12 USDA soil textural classes on the basis of the Rosetta database. Biomat thickness and saturated hydraulic conductivity are also required, and values are suggested in the spreadsheet. Bottom flux as a percentage of K(s) varied widely from 52% in the silt loam class to 2% in the sand class. To convert steady bottom flux to LTAR, a safety factor should be used, and we suggest that LTAR should be one-half of the steady bottom flux. Using these assumptions we calculated LTAR for 12 USDA soil textural classes. The LTAR ranged from 1.48 cm d−1 (0.36 gal d−1 ft−2) for the sandy clay class to 5.40 cm d−1 (1.32 gal d−1 ft−2) for the silt class." @default.
- W228141463 created "2016-06-24" @default.
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- W228141463 date "2009-01-01" @default.
- W228141463 modified "2023-09-23" @default.
- W228141463 title "Spreadsheet for Converting Saturated Hydraulic Conductivity to Long-Term Acceptance Rate tor On-Site Wastewater Systems" @default.
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- W228141463 doi "https://doi.org/10.2136/sh2009.1.0020" @default.
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