残茬覆盖对寒地旱作区土壤温度的影响

    Effect of crop residue cover on soil temperature in cold and dry farming areas

    • 摘要: 在黑龙江省西部干旱区建立不同残茬覆盖对土壤温度影响试验区,采用WQG-16.-21-61℃型曲管地温表分别测定土壤地表下5、10、15、20 cm各层温度,确定不同残茬覆盖对北方寒地旱作区土壤温度的影响规律。试验结果表明,残茬覆盖对土壤温度有明显的调节作用,5、10、15、20 cm各层有覆盖相对于无覆盖分别增温1.5~2.1℃、0.9~1.2℃、0.2~0.9、0.4~0.8℃,随着土壤层的加深,覆盖对土壤温度的调节作用越来越小。4月20日至6月15日前后,随着覆盖量的增加,土壤温度开始升高,但覆盖量增加到一定程度后,土壤温度将下降,在6月20日以后,随着覆盖量的增加,土壤温度逐渐降低,其中30%覆盖相对于无覆盖,降低1.1~1.5℃,50%~80%覆盖降低2~3.6℃,而表土层降低幅度最大,沿深度方向幅度越来越小。因此,在北方寒地农业区,考虑土壤温度这个影响因素时,完全可以进行残茬覆盖,覆盖的范围应在30%~50%之间。

       

      Abstract: For testing the effect of crop residue cover on soil temperature at various percentages of covered areas, the test plot was established in west rainless region of Heilongjiang Province. And, the soil temperatures of each layer underground 5, 10, 15, 20 cm were measured respectively by using WQG-16.-21-61℃ a knee bend ground thermometer. The testing results indicate there is a visible regulating effect in soil temperature with crop residue cover. Compared with uncovered soil, the soil temperatures of each layer were increased by 1.5~2.1℃, 0.9~1.2℃, 0.2~0.9℃, 0.4~0.8℃ respectively. The regulating effects in soil temperature were reduced with the increase of the depth of soil layer. From April 20th to June 15th, the soil temperature increased with the increase of covered amount, and decreased instead when the covered crop residue over a certain amount. After June 20th, the soil temperature decreased with the increase of covered amount, among which, the soil temperature decreased by 1.1~1.5℃, 2~3.6℃ when the covered amount 30%, 50%~80%. The decreased range is maximum on soil surface, and less and less in the direction of depth. As a result, covering with crop residue to increase the soil temperature is advisable and feasible in northern cold farming areas, in consideration of soil temperature.

       

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