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Soil compaction variation during corn growing season under conservation tillage.

机译:保护性耕作下玉米生长季土壤紧实度变化。

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Area cultivated using conservation tillage methods has recently increased in Iran and soil compaction increment is one of the most challenging issues in this new technology. In addition to the soil compaction status at the end of growing season, soil compaction variation during the growing season is also important because of its potential effect on the crop growth and yield. Therefore, soil compaction variation during the corn growing season under different tillage methods and its effect on the crop yield was investigated in this study. The research was conducted in the form of a split plot experimental design with nine treatments and six replications. Main plots were tillage methods including: (1) conventional tillage method (CT); (2) reduced tillage (RT); and (3) zero tillage or direct drilling (ZT). Soil depth ranges of 0-0.10, 0.10-0.20, and 0.20-0.30 m were considered as sub plots. Soil bulk density (BD) and soil cone index (CI) were measured during corn growth season (eight measurements for bulk density and five measurements for cone index) as indices of soil compaction. Corn silage yield, thousand kernels weight, and grain yield were also determined in this research. Collected data were analyzed using SAS statistics software and Duncan's multiple range tests were used to compare the treatments means. Results indicated that tillage methods and soil depth had a significant effect on the soil bulk density so that the maximum soil bulk density was obtained from ZT method and soil depth range of 0.10-0.20 m. The difference between soil bulk densities in different tillage methods was statistically significant from the beginning of growth season to two month after the first irrigation (sixth measurement); while, this difference was not significant from the sixth measurement to the end of growth season. Soil cone index was also significantly affected by tillage methods and soil depth in such a way that ZT method and 0.20-0.30 m soil depth range had the maximum cone index. Although, the difference between tillage methods for corn yield and yield components was not statistically different, ZT method decreased corn thousand kernels weight, silage yield, and grain yield compared to the CT method for 11.1, 2.4, and 18.2%, respectively.
机译:伊朗最近使用保护性耕作方法耕种的面积有所增加,土壤压实度增加是这项新技术中最具挑战性的问题之一。除了生长季节结束时的土壤压实状态外,生长季节期间的土壤压实度变化也很重要,因为它对作物生长和产量有潜在影响。因此,研究了不同耕作方式下玉米生长期土壤压实度变化及其对作物产量的影响。这项研究以分裂地块实验设计的形式进行,有九种处理方法和六种重复方法。主要地块为耕作方法,包括:(1)常规耕作方法(CT); (2)减耕(RT); (3)零耕种或直接钻探(ZT)。 0-0.10、0.10-0.20和0.20-0.30 m的土壤深度范围被视为子图。在玉米生长季节测量土壤容重(BD)和土壤锥度指数(CI)(对土壤密度进行八次测量,对锥度指数进行五次测量)作为土壤压实指数。这项研究还确定了玉米青贮产量,千粒重和谷物产量。使用SAS统计软件分析收集的数据,并使用Duncan的多范围测试比较治疗方法。结果表明,耕作方式和土壤深度对土壤容重有显着影响,最大土壤容重通过ZT法获得,土壤深度范围为0.10-0.20 m。从生长季节开始到第一次灌溉后两个月(第六次测量),不同耕作方法的土壤容重之间的差异具有统计学意义。而从第六次测量到生长季结束,这种差异并不明显。耕作方法和土壤深度也显着影响土壤锥指数,以ZT法和0.20-0.30 m的土壤深度范围具有最大锥指数。尽管耕作方法对玉米产量和产量构成的影响无统计学差异,但与CT法相比,ZT法分别降低了玉米千粒重,青贮产量和谷物产量,分别为11.1、2.4和18.2%。

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