From 49285cb526a891013334ddb7b8123f3e5cd8b1a7 Mon Sep 17 00:00:00 2001 From: Johannes Ranke Date: Mon, 22 Jun 2026 21:49:39 +0200 Subject: Immprove formatting --- docs/reference/GUS.html | 17 ++++++++--------- docs/reference/GUS.md | 6 +----- 2 files changed, 9 insertions(+), 14 deletions(-) (limited to 'docs/reference') diff --git a/docs/reference/GUS.html b/docs/reference/GUS.html index 949f806..0e86666 100644 --- a/docs/reference/GUS.html +++ b/docs/reference/GUS.html @@ -5,9 +5,11 @@ fontURL: "https://cdn.jsdelivr.net/npm/mathjax@3.2.2/es5/output/chtml/fonts/woff-v2" } }; - + Skip to contents @@ -42,8 +44,9 @@ equation">
-

The groundwater ubiquity score GUS is calculated according to the following -equation

+

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

@@ -144,10 +147,6 @@ be Koc values at a concentration of 1 mg/L in the water phase.

Value

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

-
-
-

Details

-

$$GUS = \log_{10} DT50_{soil} (4 - \log_{10} K_{oc})$$

References

diff --git a/docs/reference/GUS.md b/docs/reference/GUS.md index f6e4f55..8bc2a62 100644 --- a/docs/reference/GUS.md +++ b/docs/reference/GUS.md @@ -1,7 +1,7 @@ # Groundwater ubiquity score based on Gustafson (1989) The groundwater ubiquity score GUS is calculated according to the -following equation +equation \$\$GUS = \log\_{10} DT50\_{soil} (4 - \log\_{10} K\_{oc})\$\$ ## Usage @@ -101,10 +101,6 @@ print(x, ..., digits = 1) A list with the DT50 and Koc used as well as the resulting score of class GUS_result -## Details - -\$\$GUS = \log\_{10} DT50\_{soil} (4 - \log\_{10} K\_{oc})\$\$ - ## References Gustafson, David I. (1989) Groundwater ubiquity score: a simple method -- cgit v1.2.3