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首页> 外文期刊>AgroLife Scientific Journal >AGROPHYSICS QUALITY ASSESSMENT AND SOIL MOISTURE BY APPLICATION CONSERVATIVE SYSTEM OF SOIL TILLAGE NO-TILL FROM VARIOUS AGROCOENOSES IN REPUBLIC OF MOLDOVA
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AGROPHYSICS QUALITY ASSESSMENT AND SOIL MOISTURE BY APPLICATION CONSERVATIVE SYSTEM OF SOIL TILLAGE NO-TILL FROM VARIOUS AGROCOENOSES IN REPUBLIC OF MOLDOVA

机译:摩尔多瓦共和国各种农用玉米免耕免耕应用保护系统对农业物理质量和土壤水分的评估

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Conservative agricultural system is a generic term utilized to define different modalities or agricultural managementpractices to land use in view sowing crops. The purpose of this paper is to agrophysics quality assessing and soilmoisture by application of the conservative system of soil tillage No-till in Republic of Moldova. Conservation of soiltillage system offers more favorable conditions dense root system of plants (Aon et al., 2001; Barzegar et al., 2004)compared to hoes crops (maize). In this conservative system of work of carbonate chernozem (No-till) occurs waterconservation under depth of 60 cm. According to planning for the year 2016 at the experimental resort Chetrosu werefounded research polygons with conventional and conservative work of the soil - No-till within the stationary with croprotation and permanent crop - maize. Crop rotation and research variants for the agricultural years 2014-2015 and2015-2016 are presented in Table 1. Soil water reserves in the vegetation active phases of the autumn wheat were lowerin compacted layers compared to the adjacent horizons (Boincean, 2013; Rusu et al., 2013). To moisture available toplants (17-20%) compared to 12-13% of withering coefficient, soil moisture and penetration resistance negativelycorrelated (r = 0.6-0.7).
机译:保守农业系统是一个通用术语,用于定义针对播种作物的土地使用的不同方式或农业管理实践。本文的目的是通过应用摩尔多瓦共和国免耕耕作的保守系统进行农业物理质量评估和土壤水分。与土壤作物(玉米)相比,保护性耕作制度为植物的根系密集提供了更有利的条件(Aon等,2001; Barzegar等,2004)。在这种碳酸盐黑钙土(免耕)的保守工作系统中,在60厘米深度处进行了节水。根据2016年的计划,在实验胜地Chetrosu上建立了具有常规和保守土壤工作的研究多边形-静止不动的作物轮作和永久作物-玉米。表1列出了2014-2015年和2015-2016年农业年度的作物轮作和研究变化。与邻近地层相比,秋季小麦植被活跃期的土壤水分储量在压实层较低(Boincean,2013; Rusu等人)。 。,2013)。与可利用的植物水分(17-20%)相比,枯萎系数的12-13%,土壤水分和抗渗透性呈负相关(r = 0.6-0.7)。

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