地下滴灌条件下玉米土壤水分状况的形成及水分消耗

M. Romashchenko, A. Shatkovskyi, A. Sardak, Y. A. Cherevichny, N. Didenko, O. A. Marinkov
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引用次数: 1

摘要

对乌克兰草原不同地下滴灌管道(IP)方案下土壤水分形态形成特征、耗水过程及玉米产量进行了试验研究。黑栗子残咸沙土(SI "SF "Brylivske)湿润带发生了变化。随着范数的增加,相对于滴水出口的中心向土壤剖面的较深层(最高可达52 cm)移动;0-15 cm土层几乎不受潮,无论浇水速率如何。在1,0 m处,灌溉速率为2,7 m3/100 m (r. m)时湿润区关闭,而在1,4 m处,即使灌溉速率为3,7 m3/100 r. m,湿润深度达到90 cm时也未出现湿润区关闭。在灌溉量为2,7 m3/100 r. m时,黑钙质砂壤土在黄土品种(SI "SF "Velyki Klyny")上的土壤表面呈现湿润带。灌溉规范为3.7 m3/100 r. m时,最大湿润深度为70 cm,深度为25 cm时最大直径为79 cm。未观察到湿润区关闭。SI "SF "Brylivske的研究已经证实,IP的放置深度(在土壤表面或深度为30 cm)影响土壤水分状况的形成和玉米产量。滴灌(1,4 m)的最小总耗水量为6271 m3/ha,比SDI (1,4 m)高17%,比SDI (1,0 m)高29%,以DI (1,4 m)的产量最高,为15,72 t/ha。SDI (IP 1,0 m)接收了13.93 t/ha, SDI (IP 1,4 m)接收了13.50 t/ha。SDI系统1、0 m和1.4 m的IP间距对玉米产量影响不显著(分别为13.93和13.50 t/ha),但IP 1.4 m的耗水量比IP 1、0 m的耗水量减少了6.8%。SDI (IP 1.0 m)灌水量比SDI (IP 1.4 m)高13.6%。因此,就灌溉用水量和资本支出而言,SDI (IP 1,4 m)更为经济。在SI“SF”Velyki Klyny中进行的实验研究表明,IP的放置深度(在土壤表面或深度为20 cm)对玉米产量没有影响。直喷(IP 1.0 m)的产量为1.2万t/ha, SDI (IP 1.0 m)的产量为12.10 t/ha,耗水量比为533.8 m3/t,直喷(IP 1.0 m)的耗水量比为3.6%。研究结果证实了SDI系统参数对土壤水分状况形成的重要性,从而实现了作物品种和杂交品种利用SDI栽培的潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Aspects of formation of soil water regime and water consumption of corn under subsurface drip irrigation
The results of experimental researches on studying of features of formation of a water mode of soils, water consumption processes, and corn yield under different schemes of irrigation pipelines (IP) under subsurface drip irrigation (SDI) in the Steppe of Ukraine. The wetting zone of dark-chestnut residual-saline sandy soil (SI "SF "Brylivske") changed. There is a shift of the center relative to the drip water outlet into deeper horizons of the soil profile (up to 52 cm) with the increasing norm; soil layer 0-15 cm is almost not moistened, regardless of watering rate. At a distance of IP 1,0 m closing of wetting zones, occur at irrigation rates of 2,7 m3/100 running meter (r. m), and at a distance of IP 1,4 m does not occur even at irrigation rates of 3,7 m3/100 r. m, while the depth of wetting reaches 90 cm. The wetting zone of chernozem sandy loam on the loess species (SI "SF "Velyki Klyny") with irrigation rates of 2,7 m3/100 r. m was observed on the soil surface. The maximum depth of wetting, with irrigation norms of 3,7 m3/100 r. m, reached 70 cm with a maximum diameter of 79 cm at a depth of 25 cm. Closing of wetting zones was not observed. Studies at SI "SF "Brylivske" have confirmed that the depth of IP placement (on the soil surface or at a depth of 30 cm) influenced the formation of the soil water regime and the corn yield. The minimum total water consumption was 6271 m3/ha under drip irrigation (DI) (IP 1,4 m), 17 % more than SDI (IP 1,4 m), and 29% more than SDI (IP 1,0 m). The highest yield was obtained in the case of DI (IP 1,4 m) of 15,72 t/ha. SDI (IP 1,0 m) received 13,93 t/ha, and SDI (IP 1,4 m) received 13,50 t/ha. The distance between the IP in 1,0 m and 1.4 m of the SDI system did not significantly affect corn yield (13.93 and 13.50 t/ha, respectively), but at a distance of IP 1.4 m, the water consumption ratio was 6.8% less compared to IP 1,0 m. The value of the irrigation rate in the variants SDI (IP 1.0 m) was higher than SDI (IP 1,4 m) by 13,6 %. Therefore, in terms of irrigation water consumption and capital expenditures, the SDI (IP 1,4 m) is more economical. Experimental studies conducted in the SI "SF "Velyki Klyny" show that the depth of placement of IP (on the soil surface or at a depth of 20 cm) did not affect the corn yield. For DI (IP 1,0 m) the yield was 12,00 t/ha and for SDI (IP 1.0 m) was 12,10 t/ha, with a water consumption ratio of 533,8 m3/t, and for DI (IP 1,0 m) by 3,6 % more. The research results confirm the importance of the parameters of SDI system for the formation of soil water regime and, accordingly, the realization of the potential of varieties and hybrids of crops for their cultivation by SDI.
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