FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2561295890> ?p ?o ?g. }

• W2561295890 endingPage "173" @default.
• W2561295890 startingPage "161" @default.
• W2561295890 abstract "Abstract Runoff and erosion estimates are needed for rangeland management decisions and evaluation of ecosystem services derived from rangeland conservation practices. The information on the effect of scale on runoff and erosion and on the choice of runoff and erosion predictors remains scarce. The objective of this work was to evaluate the effect of scale on the selection of runoff and erosion predictors with the data from rich National Range Study database containing data from 444 coupled large (3.05 m by 9.1 m) and small (0.61 m by 1.22 m) plot field experiments. With data from both plot sizes, we assessed the usefulness of adding site-specific soil surface information to basic soil and rainfall data in order to estimate runoff and erosion in rangelands. We observed the scale-dependence of the runoff coefficient and the sediment yield. Smaller values of both variables were found at large plots as compared to small plots. Regression trees were used to build predictive relationships and evaluate the relative importance of predictors. Rainfall and basic soil properties were identified as the major predictors of runoff coefficients and sediment yields at both scales. Differences in the importance of predictors were observed between the two plot sizes and between predictions of runoff and sediment yield at the same plot sizes. The antecedent soil water content was not as important as rainfall parameters. Overall, including site-specific soil surface properties did not improve the predictability of the runoff coefficient and the sediment yield. The difference in runoff and sediment yield between small and large plots was found most likely because the small plots only contained a single soil/vegetation expression, whereas there was a matrix of vegetation clumps and bare interspaces arranged in a non-uniform pattern at the large plots. The variability of runoff and sediment yield may depend on how the latter pattern expresses itself in each of the large plots. More research or a different approach is required to account for vegetation-driven spatial hydrologic processes and their influence on rangeland runoff and soil erosion processes." @default.
• W2561295890 created "2017-01-06" @default.
• W2561295890 creator A5016877812 @default.
• W2561295890 creator A5044372161 @default.
• W2561295890 creator A5046626111 @default.
• W2561295890 creator A5076136271 @default.
• W2561295890 creator A5086723439 @default.
• W2561295890 date "2017-04-01" @default.
• W2561295890 modified "2023-09-26" @default.
• W2561295890 title "Scale effects on runoff and soil erosion in rangelands: Observations and estimations with predictors of different availability" @default.
• W2561295890 cites W1442649739 @default.
• W2561295890 cites W1490894863 @default.
• W2561295890 cites W1492543412 @default.
• W2561295890 cites W1531683302 @default.
• W2561295890 cites W1593767580 @default.
• W2561295890 cites W1632951317 @default.
• W2561295890 cites W1650359389 @default.
• W2561295890 cites W1880243058 @default.
• W2561295890 cites W196579209 @default.
• W2561295890 cites W1970507010 @default.
• W2561295890 cites W1981213426 @default.
• W2561295890 cites W1981632933 @default.
• W2561295890 cites W1986736867 @default.
• W2561295890 cites W2003972315 @default.
• W2561295890 cites W2004898026 @default.
• W2561295890 cites W2007911315 @default.
• W2561295890 cites W2008283207 @default.
• W2561295890 cites W2015629512 @default.
• W2561295890 cites W2016509674 @default.
• W2561295890 cites W2019444120 @default.
• W2561295890 cites W2020430817 @default.
• W2561295890 cites W2034695760 @default.
• W2561295890 cites W2043608216 @default.
• W2561295890 cites W2044280244 @default.
• W2561295890 cites W2046842701 @default.
• W2561295890 cites W2049474498 @default.
• W2561295890 cites W2049517593 @default.
• W2561295890 cites W2061119916 @default.
• W2561295890 cites W2063613693 @default.
• W2561295890 cites W2073839628 @default.
• W2561295890 cites W2075669838 @default.
• W2561295890 cites W2080929212 @default.
• W2561295890 cites W2083601581 @default.
• W2561295890 cites W2092795078 @default.
• W2561295890 cites W2097857034 @default.
• W2561295890 cites W2100328850 @default.
• W2561295890 cites W2107618573 @default.
• W2561295890 cites W2117259148 @default.
• W2561295890 cites W2122826475 @default.
• W2561295890 cites W2129824768 @default.
• W2561295890 cites W2130293828 @default.
• W2561295890 cites W2140668406 @default.
• W2561295890 cites W2146164655 @default.
• W2561295890 cites W2150113010 @default.
• W2561295890 cites W2156794438 @default.
• W2561295890 cites W2158814042 @default.
• W2561295890 cites W2165800593 @default.
• W2561295890 cites W2169568799 @default.
• W2561295890 cites W2179559355 @default.
• W2561295890 cites W2182526330 @default.
• W2561295890 cites W2226197050 @default.
• W2561295890 cites W2231793931 @default.
• W2561295890 cites W2238523409 @default.
• W2561295890 cites W2507409752 @default.
• W2561295890 cites W2508319885 @default.
• W2561295890 cites W2567684686 @default.
• W2561295890 doi "https://doi.org/10.1016/j.catena.2016.12.011" @default.
• W2561295890 hasPublicationYear "2017" @default.
• W2561295890 type Work @default.
• W2561295890 sameAs 2561295890 @default.
• W2561295890 citedByCount "31" @default.
• W2561295890 countsByYear W25612958902017 @default.
• W2561295890 countsByYear W25612958902018 @default.
• W2561295890 countsByYear W25612958902019 @default.
• W2561295890 countsByYear W25612958902020 @default.
• W2561295890 countsByYear W25612958902021 @default.
• W2561295890 countsByYear W25612958902022 @default.
• W2561295890 countsByYear W25612958902023 @default.
• W2561295890 crossrefType "journal-article" @default.
• W2561295890 hasAuthorship W2561295890A5016877812 @default.
• W2561295890 hasAuthorship W2561295890A5044372161 @default.
• W2561295890 hasAuthorship W2561295890A5046626111 @default.
• W2561295890 hasAuthorship W2561295890A5076136271 @default.
• W2561295890 hasAuthorship W2561295890A5086723439 @default.
• W2561295890 hasConcept C109162521 @default.
• W2561295890 hasConcept C114793014 @default.
• W2561295890 hasConcept C118518473 @default.
• W2561295890 hasConcept C123157820 @default.
• W2561295890 hasConcept C126589126 @default.
• W2561295890 hasConcept C127313418 @default.
• W2561295890 hasConcept C130989795 @default.
• W2561295890 hasConcept C159390177 @default.
• W2561295890 hasConcept C159750122 @default.
• W2561295890 hasConcept C166957645 @default.
• W2561295890 hasConcept C187320778 @default.
• W2561295890 hasConcept C18903297 @default.
• W2561295890 hasConcept C205649164 @default.
• W2561295890 hasConcept C2778755073 @default.

• next