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DYNAMICS OF HUMUS CONTENT AND AIR-WATER SOIL PROPERTIES IN INTENSIVE VEGETABLE AND FLOWER GLASSHOUSE PRODUCTION

机译:集约化蔬菜和花卉玻璃温室生产中腐殖质含量和土壤水分动力学的变化

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The investigation was conducted in Magadenovac glasshouses, eastern Croatia during seventeen years (1985. - 2002.). In that period, the glasshouse production of vegetables and flowers was intensive during the whole year. The trial was set up on 500 m2. Because of often crop rotation during the same year, soil tillage must be done fast and soil must be homogenized till depth of about 40 cm. Often in practice it is not possible to plough because of numerous reasons and then main mechanization is roto-digging machine. The aim of this investigation was to determine the consequences of long-term application of the special roto-digging machine and dynamics of organic matter and humus content during 17 years. For this purpose, multiple chemical and physical analyses were done. It was determined that, by intensive production during 17 years, organic matter content in soil surface layer significantly decreased (1995 year - 8.60% and 2002 year - 5.00%). In subsurface layer (35-50 cm) organic matter content decreased by about 50%. At the same time, by decreasing organic matter content soil became more acid, because pH value measured in 1M KCl after 17 years was by 1.4 units lower in the surface layer, and by about 0.5 units lower in subsurface layer. Finally, soil became acid (pHKCl = 4.8). Decreasing in organic matter and humus content led to soil compaction, decreased soil porosity and degradation of other physical and chemical properties. It can be concluded, that it is necessary to import complete agricultural operations relative to soil tillage for soil preserving.
机译:这项调查是在十七年(1985.-2002)期间在克罗地亚东部的Magadenovac温室进行的。在那个时期,温室里蔬菜和花卉的生产是全年密集的。审判面积为500平方米。由于同一年经常轮作农作物,必须快速进行土壤耕作,并且必须将土壤均质化直至深度约40厘米。实际上,由于多种原因,不可能进行耕作,然后主要的机械化是旋挖机。这项调查的目的是确定长期使用专用旋挖机的后果以及17年间有机物和腐殖质含量的动态变化。为此,进行了多种化学和物理分析。已确定,通过17年的集约化生产,土壤表层有机质含量显着下降(1995年-8.60%和2002年-5.00%)。在地下层(35-50厘米)中,有机物含量降低了约50%。同时,由于有机物含量的降低,土壤变得更酸,因为在17年后的1M KCl中测得的pH值在表层降低了1.4个单位,在表层降低了约0.5个单位。最后,土壤变成酸性(pHKCl = 4.8)。有机质和腐殖质含量的减少导致土壤压实,土壤孔隙率降低以及其他物理和化学性质的降低。可以得出的结论是,有必要进口与土壤耕作有关的完整的农业作业以保全土壤。

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