土壤性质对霍姆斯省部分土壤钾形态的影响

S. Shamsham, R. Nasra, Rawaa Z. Ayoush
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引用次数: 0

摘要

本研究采用标准的实验室程序确定了霍姆斯一些土壤中钾的形态(水溶性钾、交换性钾、有效钾、非交换性钾、晶格钾、总钾)。土壤是阿什拉菲亚、马拉那、穆赫塔里亚、鲁哈马、桑卡里、马斯托拉、萨达德、阿尔卡亚、格代达、赛义德。分析了样品的土壤力学组成(砂、粉、粘土)和化学组成(pH、EC、O.M),并分析了钾的不同形态。土壤中水溶性、交换性、有效态、非交换态、晶格态和全钾量;范围为1.49 - 145.92、244.46 - 787.71、245.95 - 954.83、11.10 - 836.57、3678.08 - 18041.08和4583.00 - 19643 mg/Kg。研究表明,土壤中晶格K占全钾的最大部分,而水溶性K占全钾的最低部分,全钾和晶格K与ph呈显著正相关,水溶性K浓度与有机质和砂土呈显著正相关。速效钾与沙粒呈显著正相关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of Soil Properties on forms of potassium in Some Soils of Homs Governorate
The study was conductedto determine the forms of potassium in soils (water soluble K, exchangeable K, available K, non-exchangeable K, lattice K, total K) in some of Homs soils using standard laboratory procedures. The soils were ASHRAFIA, MARANA, MOUKHTARIA, ROUGHAMA, SANKARY, MASTORAH, SADAD, ARQAYA, GDAIDA, SAYED. The samples were analyzed for mechanical composition of soil viz., sand, silt, clay and chemical composition viz., pH, EC, O.M., and analyzed the different forms of potassium. The amount of water soluble, exchangeable, available, non-exchangeable, lattice and total-K in soils; ranged from 1.49 – 145.92, 244.46 – 787.71, 245.95 – 954.83, 11.10 – 836.57, 3678.08 – 18041.08 and 4583.00 – 19643 mg/Kg. The study showed that lattice K is the largest part of total K in the soils, while the water soluble K is the lowest part of total K.The total K and lattice K showed significant and positive correlation with pH.  Water-soluble K concentrations positively correlated with organic matter and sand. The available K showed significant and positive correlation with sand.
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