Efficiency of Application of Integrated Measures To Combat Erosion With The Use of Irrigation Systems In Azerbaijan

Z. Aliyev
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Abstract

Studies in the article have shown that productivity increases with improved structure. This is explained by the fact that in soils with 0.25 mm diameter water-resistant aggregates of 14%, grain yield is 22.2 cents / ha, while water-resistant aggregates are 8%. In soils, this figure decreased to 18.4 cents / ha (3.8 cents / ha). It is also known that alfalfa plays a key role in improving the water-physical properties of the soil, as well as its agrochemical composition. The author's research shows that the amount of water-resistant aggregates under the clover is much higher than in the cotton fields. This can be clearly seen from the following comparison. Thus, the amount of water-resistant aggregates in 0-10 cm of soil in the cotton field is 4.0-18.5; While 0.5 cm is 6.5-11.2 and 20-30 cm is 4.5-18.2, in clover crops this indicator is 35.0; Increased to 24.7 and 27.0. In addition, it revealed the accumulation of more organic and mineral substances under alfalfa cultivation. They proved this by the analysis of soil samples taken from the one year and two-year plots. It was found that 1.66% humus and 0.112% total nitrogen were accumulated in the topsoil of the annual alfalfa field, while the amount of humus accumulated in the topsoil in the biennial clover field was 1.70% and the total nitrogen content was 0.150%. It should be noted. that the development of irrigation erosion in irrigated arable lands depends on the fact that the surface of the area is covered with a large cover. This was clearly shown by the observations. It was found that both relatively weak (0.4 mm / min) and very (1.4 mm / min) heavy rains protect clover soil from further washing. Thus, 0.4 mm / min. In heavy rains, the depth of the furrow under alfalfa is 14.4 mm, 31 mm at 1.4 mm / min, 50.9 and 64.2 mm between rows of cotton, respectively, and 78.6 and 113 mm along the row. 6 mm.
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阿塞拜疆利用灌溉系统防治水土流失综合措施的应用效率
文章中的研究表明,生产力随着结构的改善而提高。这可以用以下事实来解释:在直径为0.25 mm的抗水团聚体为14%的土壤中,籽粒产量为22.2分/公顷,而抗水团聚体为8%。在土壤中,这一数字降至18.4美分/公顷(3.8美分/公顷)。众所周知,紫花苜蓿在改善土壤的水物理性质及其农业化学成分方面起着关键作用。作者的研究表明,三叶草下的抗水团聚体数量远高于棉田。这可以从下面的对比中清楚地看到。因此,棉田0 ~ 10 cm土壤中抗水团聚体数量为4.0 ~ 18.5;0.5 cm为6.5-11.2,20-30 cm为4.5-18.2,三叶草作物该指标为35.0;增加到24.7和27.0。此外,紫花苜蓿栽培土壤中有机质和矿质物质积累较多。他们通过对一年和两年地块的土壤样本进行分析,证明了这一点。结果表明,一年生苜蓿草地表层土壤腐殖质积累量为1.66%,全氮含量为0.112%,二年生三叶草地表层土壤腐殖质积累量为1.70%,全氮含量为0.150%。值得注意的是。灌溉区水土流失的发生与灌溉区地表覆盖面积大有关。观察清楚地表明了这一点。研究发现,较弱(0.4 mm / min)和非常强(1.4 mm / min)的降雨都能保护三叶草土壤免受进一步的冲刷。因此,在大雨中,紫花苜蓿下的沟深为14.4毫米,在1.4毫米/分钟时为31毫米,棉花行间的沟深分别为50.9和64.2毫米,沿行深为78.6和113毫米。6毫米。
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