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Effect of mouldboard ploughing and shallow tillage on sub-soil physical properties and crop performance.

机译:翻板和浅耕对地下土壤物理性质和农作物生长性能的影响。

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摘要

This study was conducted in spring 2011 in a long-term field experiment with the objective of assessing the effect of shallow tillage (ST) and mouldboard ploughing (MP) on important soil physical properties and crop performance. Undisturbed soil samples were taken before sowing from depths of 15-20, 25-30 and 35-40 cm for the determination of saturated hydraulic conductivity (Ks), bulk density (Bd), and water retention capacity in laboratory conditions. Penetrometer resistance (PR) was measured in the field after 1 month of sowing. Plant density of barley (Hordeum vulgare) was also counted after 1 month of sowing. Field water content was significantly higher for MP than ST at 15-20 cm (MP=27%, ST=22.5%) and 25-30 cm depth (MP=29.3%, ST=24.8). Water retention at 1 m suction was also significantly higher in the treatment with MP at the depth of 25-30 cm (31%) than in the ST treatment (27.7%). Significantly higher Ks value was found for ST at depths of 15-20 (13.09 cm h-1) and 25-30 cm (5.10 cm h-1) than for MP (11.15 and 3.52 cm h-1, respectively). Soil Bd was significantly lower in MP treatments for the first two investigated depths (1.43 and 1.44 g cm-3, respectively) than in the ST (1.54 and 1.53 g cm-3). Significant higher PR value was found for ST, especially at the depth of 5-35 cm, but the result was not so high as to reduce the root growth. Water content determined parallel with PR measurement was not significantly different for the two treatments. Plant density as well as crop yield in the ST treatment was higher (3840 kg ha-1) than in the MP treatment (2490 kg ha-1). Therefore, we concluded that long-term ST treatment markedly influenced crop performance and yield by facilitating soil physical properties.
机译:这项研究是在2011年春季进行的一项长期田间试验,目的是评估浅耕(ST)和mo板犁(MP)对重要的土壤物理特性和作物生长的影响。在播种之前,从15-20、25-30和35-40 cm的深度采集未经扰动的土壤样品,以测定实验室条件下的饱和导水率(Ks),容重(Bd)和保水能力。播种1个月后,在田间测量针入度计电阻(PR)。播种1个月后,还计算了大麦(大麦)的植物密度。在15-20厘米(MP = 27%,ST = 22.5%)和25-30厘米深度(MP = 29.3%,ST = 24.8)下,MP的田间含水量显着高于ST。 MP处理深度为25-30 cm(31%)时,在1 m吸力下的保水率也显着高于ST处理(27.7%)。与MP相比,ST在15-20(13.09 cm h -1 )和25-30 cm(5.10 cm h -1 )深度处的Ks值显着高于MP (分别为11.15和3.52 cm h -1 )。在前两个调查深度(分别为1.43和1.44 g cm -3 )下,MP处理的土壤Bd显着低于ST(1.54和1.53 g cm -3 )。 >)。发现ST的PR值显着较高,尤其是在5-35 cm的深度,但结果并没有降低根系生长。两种处理与PR测量平行测定的水含量无显着差异。 ST处理(3840 kg ha -1 )的植物密度和农作物产量高于MP处理(2490 kg ha -1 )。因此,我们得出结论,长期的ST处理通过促进土壤物理特性显着影响作物的生长性能和产量。

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