Effect of Low Temperature Heating of Potassium-Depleted Soils on Secondary Potassium Release to Calcium Chloride and Wood Vinegar and Fixation

IF 1.4 4区 农林科学 Q4 SOIL SCIENCE
Mahdi Najafi-Ghiri, Hamid Reza Boostani, Soheila Sadat Hashemi
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Abstract

Potassium behavior in calcareous soils are very complex and are affected by several factors, such as the content of carbonates and soil heating. In the present research, the comparison of four calcareous soils with varying amounts of carbonates, different mineralogy, and texture (collected from Fars province, southern Iran) was compared to analyze the content of K species, K release by solutions of 0.01 M CaCl2 and 1% wood vinegar, and K re-fixation. The study also investigated the impact of heating K-depleted soils to 100°C on the secondary release and re-fixation of K. The results showed that the studied soils contained 3–60% carbonates, 14–53% clay, and a relatively similar mineral composition: smectite, illite, chlorite, palygorskite (in dry areas), and vermiculite (in humid areas). Wood vinegar extracted more K from soils with less carbonates than CaCl2, while this difference was not significant for Fluvisols, which contains about 60% carbonates. Mollic Vertisols with low carbonate content (about 3%) and high levels of clay and smectite released less K in the initial phase. However, K release by this soil decreased less in the second phase, indicating the higher buffering capacity of Mollic Vertisols in providing soluble K. Heating the soil increased the secondary release of K, but decreased the amount of K re-fixation in soils treated with CaCl2. Generally, Mollic Vertisols fixed more K than other soils. In addition, the type of extractant had no effect on the content of K fixation in the studied soils except Mollic Vertisols. However, wood vinegar reduced the K fixation content in Mollic Vertisols compared to CaCl2. In general, it can be concluded that wood vinegar can provide more K to the plants without dissolving K-bearing minerals compared to CaCl2. In addition, soil heating can influence the process of K release and fixation in K-depleted soils.

Abstract Image

低温加热缺钾土壤对氯化钙和木醋二次释放钾及固定的影响
摘要 石灰质土壤中钾的行为非常复杂,受多种因素的影响,如碳酸盐含量和土壤加热。本研究比较了四种不同碳酸盐含量、不同矿物学和质地的石灰性土壤(采集自伊朗南部法尔斯省),分析了钾物种的含量、0.01 M CaCl2 和 1%木醋溶液对钾的释放以及钾的再固定。研究还调查了将缺钾土壤加热到 100°C 对钾的二次释放和再固定的影响。研究结果表明,所研究的土壤中含有 3-60% 的碳酸盐、14-53% 的粘土,以及相对相似的矿物成分:直闪石、伊利石、绿泥石、叶腊石(干燥地区)和蛭石(潮湿地区)。与 CaCl2 相比,木醋从碳酸盐含量较少的土壤中萃取的钾更多,而对于碳酸盐含量约为 60% 的 Fluvisols 而言,这种差异并不显著。碳酸盐含量较低(约 3%)、粘土和直闪石含量较高的 Mollic Vertisols 在初始阶段释放的钾较少。加热土壤会增加钾的二次释放,但会减少用 CaCl2 处理过的土壤中钾的再固定量。一般来说,钾的固定量莫利克眩晕土比其他土壤要多。此外,萃取剂的类型对所研究土壤中的钾固定含量没有影响,但 Mollic Vertisols 土壤除外。然而,与 CaCl2 相比,木醋降低了 Mollic Vertisols 中的钾固定含量。总之,可以得出结论,与 CaCl2 相比,木醋可以在不溶解含钾矿物质的情况下为植物提供更多的钾。此外,土壤加热也会影响贫钾土壤的钾释放和固定过程。
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来源期刊
Eurasian Soil Science
Eurasian Soil Science 农林科学-土壤科学
CiteScore
2.70
自引率
35.70%
发文量
137
审稿时长
12-24 weeks
期刊介绍: Eurasian Soil Science publishes original research papers on global and regional studies discussing both theoretical and experimental problems of genesis, geography, physics, chemistry, biology, fertility, management, conservation, and remediation of soils. Special sections are devoted to current news in the life of the International and Russian soil science societies and to the history of soil sciences. Since 2000, the journal Agricultural Chemistry, the English version of the journal of the Russian Academy of Sciences Agrokhimiya, has been merged into the journal Eurasian Soil Science and is no longer published as a separate title.
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