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Effects of tillage practices on water consumption characteristics and grain yield of winter wheat under different soil moisture conditions

机译:不同土壤水分条件下耕作方式对冬小麦耗水特征和籽粒产量的影响

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A serious water shortage is threatening agricultural sustainability in the Huang-Huai-Hai Plain of China. Long-term reduced tillage (shallow rotary tillage) has led to thickening of the plough pan, which prevents the infiltration of precipitation and inhibits the root growth of wheat. Moreover, the topsoil was usually too loose to retain soil moisture. These conditions were not conducive to the highly efficient use of limited water for wheat production. The experiment was conducted from 2011 to 2013 using a split plot design. The main plots contained five different tillage treatments, and the subplots consisted of the two following different irrigation treatments: rain fed and supplemental irrigation (SI). Subsoiling promoted soil water consumption and crop evapotranspiration as well as significantly increased the water potential (psi(L)), transpiration rate (T-r) and net photosynthesis rate (P-n) of the flag leaves. Furthermore, subsoiling increased the 1000-grain weight and grain yield of winter wheat under both the rain fed and SI conditions compared with long-term rotary tillage. Subsoiling could even increase spike number under SI conditions, but could not increase the agronomic water use efficiency (AWUE). Harrowing or moderate topsoil packing before seeding increased the water content of the topsoil, the water consumption from the deep soil layers, the Pn of the flag leaves, and the 1000-grain weight, grain yield and AWUE in plots that were subsoiled. However, excessive topsoil packing significantly decreased the psi(L), T-r, P-n and water use efficiency (WUEleaf) of flag leaves as well as the 1000-grain weight, grain yield and AWUE under both the rain fed and SI conditions. (C) 2016 Elsevier B.V. All rights reserved.
机译:严重的水资源短缺正威胁着中国黄淮海平原的农业可持续发展。长期减少的耕作(浅耕)会导致犁盘加厚,这会阻止降水的渗透并抑制小麦的根系生长。此外,表层土壤通常太松散而无法保留土壤水分。这些条件不利于高效利用有限的水来生产小麦。该实验是在2011年至2013年期间使用分割图设计进行的。主要地块包含五种不同的耕作处理方式,子样地包括以下两种不同的灌溉处理方式:雨水灌溉和补充灌溉(SI)。深层耕作促进了土壤耗水量和作物蒸散,并显着提高了剑叶的水势(psi(L)),蒸腾速率(T-r)和净光合作用速率(P-n)。此外,与长期轮作相比,在雨水喂养和SI条件下,深松提高了冬小麦的1000粒重和谷物产量。在SI条件下,深耕甚至可以增加穗数,但不能提高农艺用水效率(AWUE)。播种前耙松或适度的表土堆积增加了表土的水分含量,深层土壤的耗水量,旗叶的Pn以及深层耕地的1000粒重,谷物产量和AWUE。然而,过多的表土堆积显着降低了旗叶的psi(L),T-r,P-n和水分利用效率(WUEleaf),以及在雨水和SI条件下千粒重,谷物产量和AWUE。 (C)2016 Elsevier B.V.保留所有权利。

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