{"title":"Influence of soil type and irrigation on yield of spring-sown barley and peas and autumn-sown greenfeed in Canterbury","authors":"C. M. Bennett, T. Webb","doi":"10.1080/03015521.1987.10425549","DOIUrl":null,"url":null,"abstract":"Abstract Close linear correlations were obtained between yield of spring-sown crops and evapotranspiration calculated for each of four soil types and irrigation treatments in Canterbury. Available soil water storage, derived from soil depth (which was the only soil factor used to represent soil types), was shown to be the major soil factor determining crop yield. Under dryland conditions, barley and pea yields were greatly affected by each soil's available water storage capacity. In the two driest seasons, crops grown on the deep soils yielded 2–3 times higher than those on the shallow soils. Under irrigation, soil type differences were less important and, where adequate water was supplied, crops grown on shallow soils produced yields equivalent to those from deep soils. Relative crop responses to irrigation of the different soils were dependent upon the nature of the season and the timing of irrigation. In drier seasons, whenever irrigation treatments failed to eliminate severe water deficit stress in cr...","PeriodicalId":19285,"journal":{"name":"New Zealand journal of experimental agriculture","volume":"104 1","pages":"123-133"},"PeriodicalIF":0.0000,"publicationDate":"1987-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"New Zealand journal of experimental agriculture","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/03015521.1987.10425549","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 4
Abstract
Abstract Close linear correlations were obtained between yield of spring-sown crops and evapotranspiration calculated for each of four soil types and irrigation treatments in Canterbury. Available soil water storage, derived from soil depth (which was the only soil factor used to represent soil types), was shown to be the major soil factor determining crop yield. Under dryland conditions, barley and pea yields were greatly affected by each soil's available water storage capacity. In the two driest seasons, crops grown on the deep soils yielded 2–3 times higher than those on the shallow soils. Under irrigation, soil type differences were less important and, where adequate water was supplied, crops grown on shallow soils produced yields equivalent to those from deep soils. Relative crop responses to irrigation of the different soils were dependent upon the nature of the season and the timing of irrigation. In drier seasons, whenever irrigation treatments failed to eliminate severe water deficit stress in cr...