白头菜、番茄和小麦轮作下麦秸和稻壳踏地土壤某些物理性质的变化

B. Bayraklı, C. Gülser
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引用次数: 0

摘要

为了揭示施用麦秸(WS)和稻壳(RH)后,白头菜(WHC)、番茄(T)和小麦(W)轮作中土壤某些物理性质的变化,采用粉质粘土(SiC)质地土和粉质土地(SiL)质地土进行了研究。测定每株收获后的土壤有机质(OM)、容重(BD)、总孔隙度(F)、团聚体稳定性(AS)、平均重径(MWD)、田间容量(FC)、体积含水量(Ɵ)、抗渗透能力(PR)、相对饱和度(RS)和初始入渗(In)值。试验结果表明,施用WS和RH后,收获WHC、T和W后,土壤OM含量和F值增加,BD值下降。在碳氮比较高的情况下,WS处理对土壤OM含量的增加大于RH处理。BD、AS和MWD值一般在收获后最低,而BD、AS、PR和in值一般在收获后最高。粉质粘土(SiC)质地土OM含量与BD(-0.561**)、MWD(-0.680**)、RS(-0.528**)呈极显著负相关,与BD(-0.809**)、AS(-0.543**)、MWD(-0.830**)、PR(-0.555**)呈极显著负相关,与FC(0.728**)、Ɵ(0.814**)、RS(0.767**)呈极显著正相关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Changes in some physical properties of the soils tread with wheat straw and rice husk under the rotation of white-head cabbage, tomato and wheat
This study was carried out silty clay (SiC) textured soil and silty land (SiL) textured soil in order to reveal the changes in some physical properties of the soil in white-head cabbage (WHC), tomato (T) and wheat (W) rotation after the application of wheat straw (WS) and rice husk (RH). Soil organic matter (OM), bulk density (BD), total porosity (F), aggregate stability (AS), mean weight diameter (MWD), field capacity (FC), volumetric water content (Ɵ), penetration resistance (PR), relative saturation (RS) and initial infiltration (In) values were determined, after harvest of each plant. As the results of the experiments pointed out, soil OM contents and F values increased, while BD values decreased after WHC, T and W harvest with WS and RH application. With a higher C/N ratio, WS application increased soil OM content more than RH application. The lowest BD, AS, and MWD values were generally obtained after the WHC and T harvest, and the highest BD, AS, PR and in values after the W harvest. Soil OM content showed very significant negative relationships with BD (-0.561**), MWD (-0.680**) and RS (-0.528**) in the silty clay (SiC) textured soils, while it showed very significant negative relationships with BD (-0.809**), AS (-0.543**), MWD (-0.830**), PR (-0.555**) and very significant positive relationships with FC (0.728**), Ɵ (0.814**), RS (0.767**) in the silty loam (SiL) textured soils.
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