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播种方式对旱地小麦土壤水分动态和籽粒蛋白质形成的影响。

Effects of sowing modes on soil water dynamics and grain protein formation in dryland wheat.

机构信息

College of Agriculture, Shanxi Agricultural University, Jinzhong 030801, Shanxi, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2021 Nov 15;32(11):3977-3987. doi: 10.13287/j.1001-9332.202111.030.

Abstract

In order to clarify the mechanisms underlying dryland wheat quality improvement through sowing technology, the effects of wide space sowing (WSS), furrow sowing (FS), and drill sowing (DS) on soil moisture dynamics and grain protein formation in dryland wheat field were studied in Wenxi, Shanxi Province in 2017-2018 (normal year) and 2018-2019 (dry year). The results showed that compared with the DS, FS significantly increased soil water storage in the 0-200 cm depth at anthesis stage (8.2%-18.7%), and increased the soil water storage in 0-60 cm layer during the two years, 60-120 cm layer in normal year, and 120-200 cm layer in dry year. WSS significantly increased soil water storage in 0-200 cm layer at anthesis stage in normal year (5.2%). Compared with DS, FS significantly increased water consumption of anthesis to mature stage, while WSS significantly increased water consumption from sowing to anthesis stage in dry year. Compared with DS, the glutamine synthetase (GS) activity of grains at 15-35 days after anthesis was significantly increased by FS and WSS, while the glutamate synthase (GOGAT) activity of flag leaves and grains at 5-35 days after anthesis was significantly increased by FS in the dry year. Compared with DS, FS significantly increased grain yield by 20.4%-44.8%, grain protein yield by 25%-49%, and increased grain albumin and globulin contents. WSS significantly increased grain yield by 9%-40%, and increased grain gliadin content. Under different sowing modes of dryland wheat, GS and GOGAT activities in flag leaves and grains after anthesis were significantly correlated with water consumption at anthesis to maturity stage. There were significant correlations between GS and GOGAT activities in flag leaves and grains and 0-120 cm soil layers in the normal water year, and between GS and GOGAT activities and 0-60 cm, 120-200 cm soil layers in the dry year. The contents of grain albumin, globulin and total protein were significantly correlated with soil water storage in 0-60 cm layer at anthesis stage, as well as soil water storage in 120-200 cm layer at anthesis stage in the dry year. In conclusion, FS was beneficial to increasing soil water storage at anthesis and water consumption after anthesis of dryland wheat, improving GS and GOGAT activities of flag leaf and grain, with positive consequences on yield and grain protein content. In addition, deep water storage was more conducive to quality improvement in the late growth period in the dry year.

摘要

为了阐明通过播种技术提高旱地小麦品质的机制,本研究于 2017-2018 年(正常年份)和 2018-2019 年(干旱年份)在山西闻喜研究了宽行播种(WSS)、沟播(FS)和条播(DS)对旱地小麦田间土壤水分动态和籽粒蛋白质形成的影响。结果表明,与 DS 相比,FS 显著增加了开花期 0-200cm 土层的土壤储水量(8.2%-18.7%),并增加了两年间 0-60cm 土层、正常年份 60-120cm 土层和干旱年份 120-200cm 土层的土壤储水量。WSS 显著增加了正常年份开花期 0-200cm 土层的土壤储水量(5.2%)。与 DS 相比,FS 显著增加了开花至成熟阶段的耗水量,而 WSS 显著增加了干旱年份播种至开花阶段的耗水量。与 DS 相比,FS 和 WSS 显著增加了开花后 15-35 天籽粒中谷氨酰胺合成酶(GS)的活性,而 FS 显著增加了干旱年份开花后 5-35 天旗叶和籽粒中谷氨酸合酶(GOGAT)的活性。与 DS 相比,FS 显著增加了 20.4%-44.8%的籽粒产量、25%-49%的籽粒蛋白质产量,并增加了籽粒白蛋白和球蛋白含量。WSS 显著增加了 9%-40%的籽粒产量,增加了籽粒醇溶蛋白含量。在旱地小麦的不同播种方式下,开花后旗叶和籽粒中 GS 和 GOGAT 的活性与开花至成熟阶段的耗水量显著相关。在正常水分年份,旗叶和籽粒中 GS 和 GOGAT 的活性与 0-120cm 土层显著相关,在干旱年份,旗叶和籽粒中 GS 和 GOGAT 的活性与 0-60cm、120-200cm 土层显著相关。籽粒白蛋白、球蛋白和总蛋白含量与开花期 0-60cm 土层的土壤储水量以及干旱年份开花期 120-200cm 土层的土壤储水量显著相关。综上所述,FS 有利于增加旱地小麦开花期的土壤储水量和开花后的耗水量,提高旗叶和籽粒中 GS 和 GOGAT 的活性,对产量和籽粒蛋白质含量有积极影响。此外,在干旱年份,深层储水更有利于后期生长阶段的品质提高。

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