2020
DOI: 10.1016/j.scitotenv.2020.138516
|View full text |Cite
|
Sign up to set email alerts
|

New parameters for the quantitative assessment of the proliferation of antibiotic resistance genes dynamic in the environment and its application: A case of sulfonamides and sulfonamide resistance genes

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

0
10
0

Year Published

2020
2020
2024
2024

Publication Types

Select...
6

Relationship

1
5

Authors

Journals

citations
Cited by 11 publications
(10 citation statements)
references
References 39 publications
0
10
0
Order By: Relevance
“…For PLS modeling, DT 50 derived from dissipation in nonsterile soil (reflecting overall dissipation, labeled with D) was set as a dependent variable and the difference in DT 50 between sterile and nonsterile soil (reflecting microbial degradation contribution to overall dissipation, labeled with M) and K F derived from the Freundlich isotherm model (reflecting sorption contribution to overall dissipation, labeled with K) were set as independent variables. As seen from PLS modeling results (Table S3), both determination coefficient ( R 2 = 0.777) and cross-validated determination coefficient ( Q 2 = 0.547) are higher than 0.5 and the difference between R 2 and Q 2 ( R 2 – Q 2 = 0.23) is lower than 0.3, indicating that the relationship developed is excellent due to no irrelevant terms and few outliers. , In addition, the Williams plot based on standardized residuals (δ) and leverage values ( h i ) (Figure S5) shows that δ lies between −3 and 3 and all of the h i values are lower than warning leverage h *, revealing no outliers for the response. , Consequently, the relationship developed is robust and reliable. From Table S3, the relationship between overall dissipation and biodegradation/sorption can be described with important diagnostics as follows where D represents overall dissipation of SAs in soil (i.e., DT 50 derived from dissipation in nonsterile soil), M represents microbial degradation contribution to overall dissipation (i.e., the difference in DT 50 between sterile and nonsterile soils), K represents sorption contribution to overall dissipation (i.e., K F derived from the Freundlich isotherm model), R 2 is the determination coefficient, and Q 2 is the cross-validated determination coefficient.…”
Section: Resultsmentioning
confidence: 93%
See 4 more Smart Citations
“…For PLS modeling, DT 50 derived from dissipation in nonsterile soil (reflecting overall dissipation, labeled with D) was set as a dependent variable and the difference in DT 50 between sterile and nonsterile soil (reflecting microbial degradation contribution to overall dissipation, labeled with M) and K F derived from the Freundlich isotherm model (reflecting sorption contribution to overall dissipation, labeled with K) were set as independent variables. As seen from PLS modeling results (Table S3), both determination coefficient ( R 2 = 0.777) and cross-validated determination coefficient ( Q 2 = 0.547) are higher than 0.5 and the difference between R 2 and Q 2 ( R 2 – Q 2 = 0.23) is lower than 0.3, indicating that the relationship developed is excellent due to no irrelevant terms and few outliers. , In addition, the Williams plot based on standardized residuals (δ) and leverage values ( h i ) (Figure S5) shows that δ lies between −3 and 3 and all of the h i values are lower than warning leverage h *, revealing no outliers for the response. , Consequently, the relationship developed is robust and reliable. From Table S3, the relationship between overall dissipation and biodegradation/sorption can be described with important diagnostics as follows where D represents overall dissipation of SAs in soil (i.e., DT 50 derived from dissipation in nonsterile soil), M represents microbial degradation contribution to overall dissipation (i.e., the difference in DT 50 between sterile and nonsterile soils), K represents sorption contribution to overall dissipation (i.e., K F derived from the Freundlich isotherm model), R 2 is the determination coefficient, and Q 2 is the cross-validated determination coefficient.…”
Section: Resultsmentioning
confidence: 93%
“…However, the relationship between overall dissipation and biodegradation/sorption and the relative importance of biodegradation/sorption to overall dissipation remain ambiguous. In this work, therefore, we try to solve this problem through PLS analysis aided with software SIMCA . For PLS modeling, DT 50 derived from dissipation in nonsterile soil (reflecting overall dissipation, labeled with D) was set as a dependent variable and the difference in DT 50 between sterile and nonsterile soil (reflecting microbial degradation contribution to overall dissipation, labeled with M) and K F derived from the Freundlich isotherm model (reflecting sorption contribution to overall dissipation, labeled with K) were set as independent variables.…”
Section: Resultsmentioning
confidence: 94%
See 3 more Smart Citations