Crop and Soil Responses to Rates of Lime

dc.contributor.author Pecinovsky, Kenneth
dc.contributor.author Lang, Brian
dc.date 2018-02-16T14:15:42.000
dc.date.accessioned 2020-06-30T03:49:15Z
dc.date.available 2020-06-30T03:49:15Z
dc.date.copyright Thu Jan 01 00:00:00 UTC 2015
dc.date.issued 2015-01-01
dc.description.abstract <p>Soil pH is one of the most important soil characteristics of crop production. The pH is the negative logarithm of the hydrogen ion activity of a soil. For each unit increase in pH, there is a 10 times change in acidity. A pH of 5 is 10 times more acid than a pH of 6, and 100 times more acid than a pH of 7. A soil pH greater than 7 is called alkaline or basic. A soil pH less than 7 is called acidic.</p>
dc.format.mimetype application/pdf
dc.identifier archive/lib.dr.iastate.edu/farms_reports/2192/
dc.identifier.articleid 3196
dc.identifier.contextkey 7229626
dc.identifier.s3bucket isulib-bepress-aws-west
dc.identifier.submissionpath farms_reports/2192
dc.identifier.uri https://dr.lib.iastate.edu/handle/20.500.12876/36055
dc.language.iso en
dc.relation.ispartofseries RFR A14101
dc.source.bitstream archive/lib.dr.iastate.edu/farms_reports/2192/CropSoilResponse_1.pdf|||Fri Jan 14 22:39:38 UTC 2022
dc.subject.disciplines Agricultural Science
dc.subject.disciplines Agriculture
dc.subject.disciplines Agronomy and Crop Sciences
dc.subject.disciplines Inorganic Chemicals
dc.subject.disciplines Natural Resources and Conservation
dc.subject.keywords Agronomy
dc.title Crop and Soil Responses to Rates of Lime
dc.type text
dc.type.genre report
dspace.entity.type Publication
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