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机构地区:[1]塔里木大学植物科学学院,新疆阿拉尔843300
出 处:《安徽农业科学》2013年第28期11592-11594,共3页Journal of Anhui Agricultural Sciences
基 金:国家自然科学基金项目(41161037)
摘 要:以78份土样数据对我国半荒漠地区土壤盐度指标的换算关系进行研究。结果表明,该区域土壤1∶5浸提液电导率(EC1∶5)与盐分摩尔总浓度(TEC1∶5)的换算关系为TEC1∶5=11.28×EC1∶5(r2=0.99,P<0.01),TEC1∶5与盐分质量总浓度(TDS1∶5)的关系方程为TDS1∶5=63.37×TEC1∶5(r2=0.99,P<0.01),由EC1∶5推算土壤全盐量(St)的经验方程为St=3.60×EC1∶5(r2=0.99,P<0.01)。Seventy-eight salt.affected soil samples in semi-desert areas were selected. Based on 1: 5 trical conductivity (EC1: 5 ), total electrolyte Concentration ( TEC1:5 ), total dissolved solids ( TDS1:5 ) The results showed that there were significant (r2 = 0. 99, P 〈 0.01 ) relationships between these TDS :5 = 63.37 × TEC1:5 and S, =3.60 × EC1:5. Key words 1:5 soil-toLwater extract; Soil salt soil to water extract method, data of elee- and soil salt eontenv (St) were obtained. indices such as TECI:5 = 11.28 × EC1:5, TDS1:5 = 63.37 × TEC1:5 and S1 = 3.60 × EC1:5.
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