首页> 外文期刊>Communications in Soil Science and Plant Analysis >Effect of Induced Soil Compaction on Changes in Soil Properties and Wheat Productivity under Sandy Loam and Sandy Clay Loam Soils: A Greenhouse Experiment
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Effect of Induced Soil Compaction on Changes in Soil Properties and Wheat Productivity under Sandy Loam and Sandy Clay Loam Soils: A Greenhouse Experiment

机译:沙壤土和沙质壤土下温室土壤压实诱导对土壤性质和小麦生产力变化的影响:温室试验

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The continuous use of heavy machinery and vehicular traffic on agricultural land led to an increase in soil compaction, which reduces crop yield and deteriorates the physical conditions of the soil. A pot experiment was conducted under greenhouse conditions to study the effects of induced soil compaction on growth and yield of two wheat (Triticum aestivum) varieties grown under two different soil textures, sandy loam and sandy clay loam. Three compaction levels [C0, C1, and C2 (0, 10 and 20 beatings)], two textural classes (sandy loam and sandy clay loam), and two genotypes of wheat were selected for the experiment. Results indicated that induced soil compaction adversely affected the bulk density (BD) and total porosity of soil in both sandy loam and sandy clay loam soils. Compaction progressively increased soil BD from 1.19 Mg m−3 in the control to 1.27 Mg m−3 in C1 and 1.40 Mg m−3 in C2 in sandy loam soil while the corresponding increase in BD in sandy clay loam was 1.56 Mg m−3 in C1 and 1.73 Mg m−3 in C2 compared to 1.24 Mg m−3 in the control. On the other hand, compaction tended to decrease total porosity of soil. In case of sandy loam, porosity declined by 5% and 17% in C1 and C2, respectively, and declined in sandy clay loam by 29% and 54%, respectively. Averaged over genotypes and textures, shoot length decreased by 15% and 26% at C1 and C2, respectively, and straw yield decreased by 21% and 61%, respectively. The compaction levels C1 and C2 significantly decreased grain yield by 12% and 41%, respectively, over the control. The deleterious effect of compaction was more pronounced on root elongation and root mass, and compaction levels C1 and C2 decreased root length by 47% and 95% and root mass by 41% and 114%, respectively, over the control. Response of soil texture to compaction was significant for almost all the parameters, and the detrimental effects of soil compaction were greater in sandy clay loam compared to sandy loam soil. The results from the experiment revealed that soil compaction adversely affected soil physical conditions, thereby restricting the root growth, which in turn may affect the whole plant growth and grain yield. Therefore, appropriate measures to avoid damaging effects of compaction on soil physical conditions should be practiced. These measures may include soil management by periodic chiseling, controlled traffic, conservation tillage, addition of organic manures, and incorporating crops with deep tap root systems in a rotation cycle.View full textDownload full textKeywordsCompaction, grain protein, root development, soil texture, wheat, yield componentsRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/00103624.2012.711877
机译:在农业用地上持续使用重型机械和车辆交通导致土壤紧实度增加,这降低了农作物的产量并恶化了土壤的物理条件。在温室条件下进行了盆栽试验,研究了土壤致密化对两种不同土壤质地(沙壤土和砂质壤土)下生长的两种小麦(Triticum aestivum)生长和产量的影响。三种压实级别[C 0 ,C 1 和C 2 (0、10和20跳动)],两个纹理级别(桑迪壤土)和沙质壤土),并选择了两种基因型的小麦。结果表明,在砂壤土和砂质壤土中,诱导的土壤压实对土壤的容重(BD)和总孔隙度有不利影响。压实使土壤BD从对照中的1.19 Mg m â3’sup>逐渐增加到C 1 和1.40中的1.27 Mg m â3’sup>砂壤土中C 2 中的Mg m â3,而砂壤土中BD的相应增加为1.56 Mg m ˆ3 C 1 中的sup>和C 2 中的1.73 Mg m →3 ,而1.24 Mg m →3 < / sup>。另一方面,压实倾向于降低土壤的总孔隙率。对于沙壤土,C 1 和C 2 的孔隙度分别下降了5%和17%,而沙质壤土的孔隙度分别下降了29%和54%,分别。按基因型和质地平均,C 1 和C 2 的茎长分别降低了15%和26%,秸秆产量分别降低了21%和61% 。与对照相比,压实水平C 1 和C 2 分别使籽粒产量分别降低12%和41%。压实对根伸长和根质量的有害影响更为明显,压实水平C 1 和C 2 降低了根长47%和95%,根质量降低了分别比对照组高41%和114%。在几乎所有参数下,土壤质地对压实的响应均很显着,并且与砂壤土相比,砂质壤土的土壤压实有害作用更大。实验结果表明,土壤压实对土壤物理条件产生不利影响,从而限制了根系的生长,进而可能影响整株植物的生长和籽粒产量。因此,应采取适当措施避免压实对土壤物理条件的破坏作用。这些措施可能包括通过定期凿土,控制交通,保护性耕作,添加有机肥料以及在轮作周期中将具有深部水龙头根系的农作物纳入土壤管理,以查看整固关键词,紧实度,谷物蛋白,根系发育,土壤质地,小麦,收益成分相关var addthis_config = {ui_cobrand:“泰勒和弗朗西斯在线”,servicescompact:“ citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,更多”,发布号:“ ra-4dff56cd6bb1830b”} ;添加到候选列表链接永久链接http://dx.doi.org/10.1080/00103624.2012.711877

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