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Evaluation of the Soil Conservation Service curve number methodology using data from agricultural plots

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dc.contributor.author Lal, Mohan
dc.contributor.author Mishra, S. K.
dc.contributor.author Pandey, Ashish
dc.contributor.author Pandey, R. P.
dc.contributor.author Meena, Pramod K.
dc.contributor.author Chaudhary, Anubhav
dc.contributor.author Jha, Ranjit Kumar
dc.contributor.author Shreevastava, Ajit K.
dc.contributor.author Kumar, Yogendra
dc.date.accessioned 2019-10-03T11:12:19Z
dc.date.available 2019-10-03T11:12:19Z
dc.date.issued 2017
dc.identifier.citation Hydrogeology Journal February 2017, Volume 25, Issue 1, pp 151–167 en_US
dc.identifier.uri http://117.252.14.250:8080/jspui/handle/123456789/3676
dc.description.abstract The Soil Conservation Service curve number (SCS-CN) method, also known as the Natural Resources Conservation Service curve number (NRCS-CN) method, is popular for computing the volume of direct surface runoff for a given rainfall event. The performance of the SCS-CN method, based on large rainfall (P) and runoff (Q) datasets of United States watersheds, is evaluated using a large dataset of natural storm events from 27 agricultural plots in India. On the whole, the CN estimates from the National Engineering Handbook (chapter 4) tables do not match those derived from the observed P and Q datasets. As a result, the runoff prediction using former CNs was poor for the data of 22 (out of 24) plots. However, the match was little better for higher CN values, consistent with the general notion that the existing SCS-CN method performs better for high rainfall–runoff (high CN) events. Infiltration capacity (fc) was the main explanatory variable for runoff (or CN) production in study plots as it exhibited the expected inverse relationship between CN and fc. The plot-data optimization yielded initial abstraction coefficient (λ) values from 0 to 0.659 for the ordered dataset and 0 to 0.208 for the natural dataset (with 0 as the most frequent value). Mean and median λ values were, respectively, 0.030 and 0 for the natural rainfall–runoff dataset and 0.108 and 0 for the ordered rainfall–runoff dataset. Runoff estimation was very sensitive to λ and it improved consistently as λ changed from 0.2 to 0.03. en_US
dc.language.iso en en_US
dc.publisher Springer en_US
dc.subject Agricultural en_US
dc.subject Curve number en_US
dc.subject Initial abstraction coefficient en_US
dc.subject India en_US
dc.subject Infiltration capacity en_US
dc.title Evaluation of the Soil Conservation Service curve number methodology using data from agricultural plots en_US
dc.type Article en_US


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