白云岩灰岩和有机肥对有机溶胶理化性质和结构的影响

P. Cairo, J. M. Armas, Bladimir Díaz Martín, Oralia Rodríguez López
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摘要

施用天然矿肥和有机肥可提高土壤生产力。这项工作是在古巴萨瓜格兰德市维拉克拉拉省北海岸的Vertisols甘蔗区进行的,目的是评估白云岩石灰石和有机肥对Vertisol一些物理化学性质的影响。在白云岩灰岩水平下,施用有机肥(4 t hm -1堆肥,15 t hm -1甘蔗滤饼)和氮磷钾(NPK)。使用的设计是条纹块。处理后8个月、19个月和36个月的土壤分析数据分别为0 ~ 20和20 ~ 40 cm。评估了以下指标:结构因子、渗透率、稳定团聚体、塑性、T值和交换阳离子。Ca/Mg比值最大值为2.58,表明处理对可交换阳离子的影响。白云岩灰岩及其与有机肥的组合对表层和底土的土壤结构和稠度均有显著的正向影响,其影响持续时间可达36个月。结果表明,结构指标类别由常规到优异(渗透率1.50 ~ 2.40),由塑性到中塑性(塑性指数36.64 ~ 13.72)的变化。
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Effect of dolomitic limestone and organic fertilizers on some physical-chemical properties and the structure of a Vertisol
The application of natural mineral and organic fertilizers can increase soil productivity. The work was carried out in Vertisols sugarcane areas on the North coast of the province of Villa Clara, municipality of Sagua la Grande, Cuba, with the objective of assessing the effect of dolomitic limestone and organic fertilizers on some physical-chemical properties of a Vertisol. An experiment was conducted with dolomitic limestone levels and combinations of organic fertilizers (4 t ha-1 compost, 15 t ha-1 sugarcane filter cake) and fertilizers (NPK). The design used was stripe blocks. The soil analysis data used at the depth of 0-20 and 20-40 cm were at 8, 19 and 36 months after application of the treatments. The following indicators were evaluated: structure factor, permeability, stable aggregates, plasticity, T value, and exchangeable cations. The Ca/Mg ratio reached a maximum value of 2.58, which shows in the effect of the treatments on the interchangeable cations. Dolomitic limestone and its combinations with organic fertilizers showed significant positive effects on soil structure and consistency, both in the surface layer and in the subsoil, with residual impact over time up to 36 months. The results obtained showed a change in the category of structural indicators from regular to excellent (permeability 1.50-2.40) and from plasticity to moderately plastic (Plastic index 36.64 -13.72)
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