Effects of Different Tillage Layer Structures on Soil Compaction and Soil Water Content
Liu Wu-re
Abstract
Liu Wu-re
Abstract
The experiments were designed in the middle black soil zone of Jilin province. The results showed that the difference of soil compaction of different treats were significant from 0 to 20 cm in profile of soil. The difference of treatments was not significant from 21 cm to 45 cm. Through comparison of different treatments with the average of soil compaction from 0 to 45 cm, soil compaction of MJHJ with ridge was most hardness, MJHJ with plain and conventional tillage were secondary. Soil water content was increased with depth from 0 to 30 cm, but it was decreased with depth from 31 cm to 60 cm. The soil water content of MJHS was higher than conventional tillage at every depth of soil layer from 0 to 60 cm, the difference was significant(P0.05). So, MJHS tillage could decrease soil compaction, increase soil water content, improve soil structure, moderate water and air in the soil.
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The experiments were designed in the middle black soil zone of Jilin province. The results showed that the difference of soil compaction of different treats were significant from 0 to 20 cm in profile of soil. The difference of treatments was not significant from 21 cm to 45 cm. Through comparison of different treatments with the average of soil compaction from 0 to 45 cm, soil compaction of MJHJ with ridge was most hardness, MJHJ with plain and conventional tillage were secondary. Soil water content was increased with depth from 0 to 30 cm, but it was decreased with depth from 31 cm to 60 cm. The soil water content of MJHS was higher than conventional tillage at every depth of soil layer from 0 to 60 cm, the difference was significant(P0.05). So, MJHS tillage could decrease soil compaction, increase soil water content, improve soil structure, moderate water and air in the soil.
Key concepts: Tillage, Compaction, Soil compaction, Water content, Environmental science, Soil water, Soil horizon, Soil science