From 3bb842b93107dd6207610de1fe5b44be66779e4d Mon Sep 17 00:00:00 2001 From: Johannes Ranke Date: Thu, 25 Apr 2019 10:25:56 +0200 Subject: Remove leftover docs from earlier version Docs now live in docs/ --- inst/web/GUS.html | 160 ------------------------------------------------------ 1 file changed, 160 deletions(-) delete mode 100644 inst/web/GUS.html (limited to 'inst/web/GUS.html') diff --git a/inst/web/GUS.html b/inst/web/GUS.html deleted file mode 100644 index a330be2..0000000 --- a/inst/web/GUS.html +++ /dev/null @@ -1,160 +0,0 @@ - - - - -GUS. pfm 0.3-7 - - - - - - - - - - - - - - - - - -
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Groundwater ubiquity score based on Gustafson (1989)

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Usage

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GUS(...)
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"GUS"(DT50, Koc, ...)
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"GUS"(chent, degradation_value = "DT50ref", lab_field = "laboratory", redox = "aerobic", sorption_value = "Kfoc", degradation_aggregator = geomean, sorption_aggregator = geomean, ...)
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"print"(x, ..., digits = 1)
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Arguments

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...
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Included in the generic to allow for further arguments later. Therefore -this also had to be added to the specific methods.
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DT50
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Half-life of the chemical in soil. Should be a field -half-life according to Gustafson (1989). However, leaching to the sub-soil -can not completely be excluded in field dissipation experiments and Gustafson -did not refer to any normalisation procedure, but says the field study should -be conducted under use conditions.
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Koc
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The sorption constant normalised to organic carbon. Gustafson -does not mention the nonlinearity of the sorption constant commonly -found and usually described by Freundlich sorption, therefore it is -unclear at which reference concentration the Koc should be observed -(and if the reference concentration would be in soil or in porewater).
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chent
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If a chent is given with appropriate information present in its -chyaml field, this information is used, with defaults specified below.
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degradation_value
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Which of the available degradation values should -be used?
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lab_field
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Should laboratory or field half-lives be used? This -defaults to lab in this implementation, in order to avoid -double-accounting for mobility. If comparability with the original GUS -values given by Gustafson (1989) is desired, non-normalised first-order -field half-lives obtained under actual use conditions should be used.
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redox
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Aerobic or anaerobic degradation data
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sorption_value
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Which of the available sorption values should be used? -Defaults to Kfoc as this is what is generally available from the European -pesticide peer review process. These values generally use a reference -concentration of 1 mg/L in porewater, that means they would be expected to -be Koc values at a concentration of 1 mg/L in the water phase.
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degradation_aggregator
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Function for aggregating half-lives
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sorption_aggregator
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Function for aggregation Koc values
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x
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An object of class GUS_result to be printed
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digits
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The number of digits used in the print method
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Value

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-A list with the DT50 and Koc used as well as the resulting score - of class GUS_result -

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Description

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The groundwater ubiquity score GUS is calculated according to -the following equation -$$GUS = \log_{10} DT50_{soil} (4 - \log_{10} K_{oc})$$

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References

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Gustafson, David I. (1989) Groundwater ubiquity score: a simple -method for assessing pesticide leachability. Environmental -toxicology and chemistry 8(4) 339–57.

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Author

- -Johannes Ranke - - -
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