2003
DOI: 10.1002/ps.765
|View full text |Cite
|
Sign up to set email alerts
|

Modelling approaches to compare sorption and degradation of metsulfuron‐methyl in laboratory micro‐lysimeter and batch experiments

Abstract: Results of laboratory batch studies often differ from those of outdoor lysimeter or field plot experiments--with respect to degradation as well as sorption. Laboratory micro-lysimeters are a useful device for closing the gap between laboratory and field by both including relevant transport processes in undisturbed soil columns and allowing controlled boundary conditions. In this study, sorption and degradation of the herbicide metsulfuron-methyl in a loamy silt soil were investigated by applying inverse modell… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

2
11
0

Year Published

2004
2004
2020
2020

Publication Types

Select...
5
3

Relationship

0
8

Authors

Journals

citations
Cited by 13 publications
(13 citation statements)
references
References 16 publications
(21 reference statements)
2
11
0
Order By: Relevance
“…This was different for the nonsterile treatments (see below), where both the RES and NER fractions showed pronounced initial sorption. This behavior is also reported in the literature for SDZ (e.g., Schmidt et al, 2008; Junge et al, 2011) and for other organic contaminants (Heistermann et al, 2003).…”
Section: Resultssupporting
confidence: 85%
“…This was different for the nonsterile treatments (see below), where both the RES and NER fractions showed pronounced initial sorption. This behavior is also reported in the literature for SDZ (e.g., Schmidt et al, 2008; Junge et al, 2011) and for other organic contaminants (Heistermann et al, 2003).…”
Section: Resultssupporting
confidence: 85%
“…Rapid movement of metsulfuron-methyl in soil, as we found to occur at the Cumberland Plateau study site, has been reported for several soils and in glacial till subsoil (Heistermann et al, 2003;Jorgensen et al, 2002;Ismail and Tet-Vun, 2003). The organic carbon and other components of the soil at our study site exhibited very low affinity in retaining the herbicides.…”
Section: Discussionsupporting
confidence: 69%
“…The organic carbon and other components of the soil at our study site exhibited very low affinity in retaining the herbicides. The rapid transport through the soil may also be attributed to "multi-domain" flow, or movement of water through "macro-pores" in the soil produced by earthworms, decaying roots and other sources (Heistermann et al, 2003;Jorgensen et al, 2002). As noted in the introduction, imazapyr and metsulfuron-methyl are similar in terms of soil retention and water solubility, hence the similar rate of transport observed for the two compounds is expected.…”
Section: Discussionmentioning
confidence: 85%
“…The measured BTCs were evaluated using equilibrium (seven cases) or kinetic models (nine cases). The studies include chlorsulfuron (Veeh et al, 1994, four studies), isoproturon (Lennartz, 1999, one study; Besien et al, 2000; one study; Pot et al, 2005, two experiments), ETD (Dressel, 2003, four experiments), picloram (Gaber et al, 1992, one experiment), metsulfuron‐methyl (Heistermann et al, 2003, one experiment), simazine (Poletika et al, 1995, one experiment), and TBA (Lennartz, 1999, one experiment).…”
Section: Resultsmentioning
confidence: 99%
“…In case of equilibrium sorption, a linear model (Henry isotherm) written as S=KnormaldCor a nonlinear model in the form of the Freundlich equation has been used in literature: S=KnormalfCnwhere S is the sorbed mass (M M −1 ), C the solute concentration (M L −3 ), K d the distribution coefficient (L 3 M −1 ), K f the Freundlich sorption constant (M 1−n L 3n M −1 ), and n the Freundlich exponent. An overview of the type of isotherm used to fit the sorption constants from batch experiments is shown in Table 1 Some sorption constants were derived from sorption kinetic studies using a two‐site nonequilibrium sorption model (e.g., Gaston and Locke, 2000) or a two‐site nonequilibrium model that includes the formation of bound residues (Gaston and Locke, 1994; Heistermann et al, 2003). In these cases, the K d coefficients represented the equilibrium sorption to all kinetic sorption sites.…”
Section: Deriving Sorption Parameters From Batch and Column Studiesmentioning
confidence: 99%