安徽农学通报
安徽農學通報
안휘농학통보
AUHUI AGRICULTURAL SCIENCE BULLETIN
2012年
10期
35-37
,共3页
李孝良%纵艳芝%于群英%段立珍%汪建飞
李孝良%縱豔芝%于群英%段立珍%汪建飛
리효량%종염지%우군영%단립진%왕건비
土壤%表面电荷%土壤性质%沿淮地区
土壤%錶麵電荷%土壤性質%沿淮地區
토양%표면전하%토양성질%연회지구
Soil%Soil surface charge%Soil property%The region along Huaihe river
用Mechlich法研究沿淮地区几种类型土壤的电荷数量,结果表明:不同类型土壤电荷数量、电荷性质存在明显差异。供试土壤负电荷量大于土壤正电荷量,土壤永久负电荷量大于可变负电荷量。在沿淮几种土壤中,黄棕壤、黄褐土CECv/CEC8.2≥0.4,为可变电荷土壤,潮土和砂姜黑土为恒电荷土壤。土壤性质是土壤表面电荷的主要影响因素,CECv和CEC8.2主要受土壤pH和粘粒含量的影响,AEC主要受土壤有机质的影响。
用Mechlich法研究沿淮地區幾種類型土壤的電荷數量,結果錶明:不同類型土壤電荷數量、電荷性質存在明顯差異。供試土壤負電荷量大于土壤正電荷量,土壤永久負電荷量大于可變負電荷量。在沿淮幾種土壤中,黃棕壤、黃褐土CECv/CEC8.2≥0.4,為可變電荷土壤,潮土和砂薑黑土為恆電荷土壤。土壤性質是土壤錶麵電荷的主要影響因素,CECv和CEC8.2主要受土壤pH和粘粒含量的影響,AEC主要受土壤有機質的影響。
용Mechlich법연구연회지구궤충류형토양적전하수량,결과표명:불동류형토양전하수량、전하성질존재명현차이。공시토양부전하량대우토양정전하량,토양영구부전하량대우가변부전하량。재연회궤충토양중,황종양、황갈토CECv/CEC8.2≥0.4,위가변전하토양,조토화사강흑토위항전하토양。토양성질시토양표면전하적주요영향인소,CECv화CEC8.2주요수토양pH화점립함량적영향,AEC주요수토양유궤질적영향。
Using the method of Mechlich, the characteristics of soil surface charge in the region along Huaihe River in Anhui Province were studied. The results showed that: There had significant difference of soil surface charge in different soil types. Generally speaking, the negative charge quantity was higher than the positive charge quantity, and the permanent negative charge was higher than variable negative charge in the tested soils. In the tested soil types, Yellow brown soil and Yellow cinnamon soil were variable charge soil, and moisturesoil and Shajiang black soil were constant charge soil. The major influencing factors of soil surface charge were soil properties. Soil pH value and clay particles were major influencing factors of soil CECv and CEC8.2, and Soil organic matter content was major influencing factor of soil AEC.