Reserves of productive water in the soil for growing winter wheat

Ya. P. Makuch, S. O. Remeniuk, V. M. Riznyk, S. O. Bondar, S. I. Vlasenko, K. M. Kopchuk
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Abstract

An analysis of the productive water reserves in the soil at the time of sowing and harvesting of winter wheat cultivated after different preceding crops was carried out. The worst conditions for the water accumulation in the 0–30 cm, 0–50 cm, and 0–100 cm soil layers were created after pea for grain — 5.3 mm, 8.7 mm, and 21.6 mm, respectively, in the soil layers; after soybean — 6.0 mm, 11.7 mm and 28.1 mm, respectively; corn for silage — 4.5 mm, 7.4 mm and 13.3 mm, respectively. Earthing the rye and oat mix and green manure made it possible to accumulate 32.9 mm and 29.9 mm of productive water reserve in the 0–100 cm layer, which can be explained by the earlier clearance of the field before the time of sowing winter wheat. In the link of crop rotation with bare fallow, the reserve of productive water in the 0–100 cm soil layer were the highest and amounted to 74.4 mm, which exceeded the link with corn for silage 5.6 times, with pea for grain and perennial grasses 2.6 and 3.4 times. In the link with soybean, the reserve of productive water in the 0–100 cm soil layer amounted to 28.1 mm, which can be explained by the low yield of this crop in this zone. It should also be taken into account that of all the studied preceding crops, soybean is harvested the latest; therefore, it is not always possible to prepare the soil well for sowing winter wheat. During the period of harvesting winter wheat, the reserve of productive water in the soil depended less on preceding crop. At the same time, in the 0–100 cm soil layer, the highest reserves of productive water were formed in the of crop rotation links with bare fallow — 41.1 mm, perennial grasses — 33.6 mm, vetch and oat mix for green manure and green fodder — 29.3 and 31.4 mm, respectively; the lowest — in the links with pea for grain, soybean and corn for silage: 26.5, 26.9, and 24.9 mm, respectively. The yield of winter wheat in the link with bare fallow was 6.52 t/ha, which by 0.80–0.99 t/ha exceeded the other links of crop rotation.
土壤中用于种植冬小麦的生产性水分储备
对不同前茬栽培的冬小麦在播种和收获时的土壤生产水分储量进行了分析。0-30 cm、0-50 cm和0-100 cm土层水分积累条件最差的土层分别为籽粒- 5.3 mm、8.7 mm和21.6 mm;大豆后-分别为6.0 mm、11.7 mm和28.1 mm;青贮玉米-分别为4.5 mm、7.4 mm和13.3 mm。黑麦与燕麦混作和绿肥在0 ~ 100 cm土层积累了32.9 mm和29.9 mm的生产水分储备,这可以解释为在冬小麦播种前较早地清理了田地。在轮作休耕环节,0 ~ 100 cm土层生产水储量最高,达74.4 mm,分别是玉米青贮环节的5.6倍、豌豆籽粒环节的2.6倍和多年生牧草环节的3.4倍。在与大豆的联系中,0-100 cm土层的生产水储量为28.1 mm,这可以解释为该区域该作物产量低。还应考虑到,在所有研究过的前面的作物中,大豆是收获最晚的;因此,播种冬小麦时不可能总是准备好土壤。在冬小麦收获期间,土壤中生产性水分的储备对前茬作物的依赖程度较低。同时,在0 ~ 100 cm土层,作物轮作环节的生产水储量最高,分别为裸休耕41.1 mm、多年生禾草33.6 mm、混作绿肥和青饲料的豌豆和燕麦29.3 mm和31.4 mm;籽粒用豌豆、青贮用大豆和玉米最低,分别为26.5、26.9和24.9毫米。光休环节冬小麦产量为6.52 t/ha,比轮作其他环节高出0.80 ~ 0.99 t/ha。
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