不同土壤和气候带下降雪对冬小麦产量的影响

P. Tarasenko, V. Tarbaev, D. Vasilieva, M. Morozov
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摘要

在气候持续变暖和人类活动对土地资源影响日益加剧的情况下,利用水土保持技术就显得尤为重要。积雪对农业具有重要意义,它改变下垫面辐射和热平衡,保护土壤不降温,防止冬季作物冻结,积累冬季降水,是干旱和半干旱区春季增加土壤水分储备的最重要来源。冬季降水占全年正常值的30%。在潮湿的夏季,在它们的帮助下形成的土壤水分储备占粮食作物产量形成总耗水量的42%,在干燥的夏季高达75%。本文旨在研究不同的保雪方法和积雪高度对粮食作物产量的影响。冬春作物收获后留高茬是一种有效的防雪方法。在高度为0.30-0.35 m的草原地区,每隔4.5 m留下高度为0.35-0.40 m、宽度为1.5 m的残茬灌木,可以积累坚实的积雪,提高小麦产量。涉水区提供了比林带更均匀的积雪分布。气候变化导致了雪的滞留成为一个紧迫的问题,不仅在干燥的草原,而且在北方甚至在森林草原。在位于萨拉托夫地区西部Balashovsky区的Vetelny国营农场进行了缓雪器的创建,该农场位于草原地带,黑土土壤在土壤覆盖层中占主导地位。在秋季设置雪障,在冬季研究其对积雪的影响。在干旱区、草原区和森林草原区比较了冬小麦生长季积雪屏障对土壤水分积累的影响。结果表明,在冬小麦再生过程中,0 ~ 1.0 m土层的生产水分储量在干草原区最少,为1377 m·ha,在森林草原区最高,达1841 m·ha。积雪滞留使干草原、草原和森林草原区土壤含水量分别增加了251、151、115 ~ 131 m·ha,分别增加了18、10、6 ~ 8%。因此,合理利用冬季降水是提高农业景观生产力的重要储备,特别是在干旱草原地区。
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Snow melioration effect on winter wheat yields in different soil and climatic zones
Under conditions of ongoing climate warming and increasing anthropogenic impact on land resources, the use of moisture-saving soil-protecting technologies becomes especially important. Snow cover is of great importance for agriculture, as it changes radiation and thermal balance of underlying surface, protecting soil from cooling and winter crops from freezing, accumulates winter precipitation, being the most important source of increasing soil moisture reserves in arid and subarid zones in spring. Winter precipitation accounts for up to 30% of the annual norm. Soil moisture reserves formed with their help take up to 42% in total water consumption for grain crop yield formation during wet summer and up to 75% during dry summer. This article aims to study the effect of different methods of snow retention and snow cover height on the yield of grain crops. An effective method of snow retention is leaving high stubble after harvesting winter and spring crops. Leaving stubble bushes with a height of 0.35-0.40 m and a width of 1.5 m every 4.5 m provides accumulation of a solid snow cover in steppe areas with a height of 0.30-0.35 m, which increases the yield of wheat. Waders provide a more uniform distribution of snow cover than forest strips. Climate change contributes to the fact that snow retention becomes an urgent problem not only in the dry steppe, but also to the north even in the forest-steppe. Creation of snow retarders was done on Vetelny state farm, located in Balashovsky district in the western part of Saratov region, in the steppe zone, where chernozem soils prevail in the soil cover. In the autumn period, snow barriers were installed, and in the winter period, their effect on snow accumulation was studied. The study of the effect of snow barriers on soil moisture accumulation during the growing season of winter wheat was compared in the zones of dry steppe, steppe and forest-steppe. It was revealed that during regrowth of winter wheat the least amount of productive moisture stocks in 0-1.0 m soil layer was contained in dry steppe 1377 m·ha, the highest in forest-steppe zone up to 1841 m·ha. Snow retention increased the amount of moisture in the soil in the dry steppe, steppe and foreststeppe zone by 251, 151, 115-131 m·ha, or 18, 10, 6-8%, respectively. Thus, rational use of winter precipitation is a significant reserve of agricultural landscape productivity increase, especially in dry-steppe areas.
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