通过搅拌和萃取改性,提高了土壤中阳离子交换容量和交换性碱性阳离子的测定效率

Jinhua Yuan, E. Shengzhe, Xinnan Zhao
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For sodic soil, the measured CEC was above the certified range, the exch. Mg and K below the certified range; the extracted Ca can be assumed the exch. Ca; the exch. Na can be calculated as CEC-(exch. Ca + exch. Mg + exch. K). The difference of CEC between measured and certified values were mainly because of the discrepancy of extractant pHs. The addition of CaCO<ce:inf loc=\"post\">3</ce:inf> (≤ 80 %) had no effect on CEC or exch. base cations’ determinations. The CaCO<ce:inf loc=\"post\">3</ce:inf> and CaSO<ce:inf loc=\"post\">4</ce:inf>∙2 H<ce:inf loc=\"post\">2</ce:inf>O combination only affected the determination of exch. 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引用次数: 0

摘要

六氨合氯化钴([Co(NH3)6]Cl3)法提取可交换(exch.)对于含有碳酸钙的土壤,可使用方解石饱和的 [Co(NH3)6]Cl3 溶液来测定交换性碱阳离子。钙。方解石饱和 [Co(NH3)6]Cl3 溶液的配制时间需要过夜。本研究评估了使用搅拌改良法制备 [Co(NH3)6]Cl3 溶液的等效性。该改良方法大大节省了时间,整个萃取时间可缩短至 3-5 分钟。在测量含有碳酸钙的土壤时,可以省略制备方解石饱和[Co(NH3)6]Cl3 溶液的步骤。对于酸性土壤,所测得的 CEC 值低于认证范围,exch.Ca、Na 和 K 均在认证值范围内;exch.镁高于认证范围。对于神经性土壤,测得的 CEC、exch.钙、镁、钠和钾均在认证值范围内。对于碱性土壤,测得的 CEC 值高于认证值范围,exch.钙、镁、钠和钾均在认证范围内。对于盐碱土,测得的 CEC 值高于认证范围,钙、镁、钠和钾的交换量低于认证范围。镁和钾的交换量低于认证范围;精确的钙和钠交换量即使在盐碱地中也无法实现。由于石膏和钠盐的溶解,即使在如此短的提取时间内也无法实现 Ca 和 Na 的准确交换。对于含钠土壤,测得的 CEC 值高于认证范围,exch.镁和钾低于认证范围;萃取的钙可以认为是 exch.Ca;exch.Na 可按 CEC-(exch.Ca+exch.Mg+exch.K)计算。测量值与认证值之间的 CEC 差异主要是由于萃取剂 pH 值的差异造成的。添加 CaCO3(≤ 80%)对 CEC 或碱式阳离子交换值的测定没有影响。CaCO3 和 CaSO4∙2 H2O 的组合仅影响 exch.Ca
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Improved determination efficiency of the cation exchange capacity and exchangeable base cations in soil using stirring and extraction modifications
The hexamminecobalt trichloride ([Co(NH3)6]Cl3) method extracts exchangeable (exch.) base cations needing 60 min. For soils containing calcium carbonate, a calcite saturated [Co(NH3)6]Cl3 solution is used to determine the exch. Ca. The preparing time of calcite saturated [Co(NH3)6]Cl3 solution requires to set overnight. This study evaluated the equivalence of [Co(NH3)6]Cl3 method using stirring modification. The proposed modification can vastly save time and the whole extraction time can be shortened to 3–5 min. The preparing calcite saturated [Co(NH3)6]Cl3 solution procedure can be omitted when measured soils containing calcium carbonate. For acidic soil, the measured CEC was below the certified range, the exch. Ca, Na and K were all in the certified value range; the exch. Mg above the certified range. For neural soil, the measured CEC, exch. Ca, Mg, Na and K were all in the certified range. For alkaline soil, the measured CEC was above the certified range, the exch. Ca, Mg, Na and K were all in the certified range. For saline soil, the measured CEC was above the certified range, the exch. Mg and K below the certified range; accurate exch. Ca and Na could not be achieved even in such a short extraction time because of the dissolution of gypsum and sodium salts. For sodic soil, the measured CEC was above the certified range, the exch. Mg and K below the certified range; the extracted Ca can be assumed the exch. Ca; the exch. Na can be calculated as CEC-(exch. Ca + exch. Mg + exch. K). The difference of CEC between measured and certified values were mainly because of the discrepancy of extractant pHs. The addition of CaCO3 (≤ 80 %) had no effect on CEC or exch. base cations’ determinations. The CaCO3 and CaSO4∙2 H2O combination only affected the determination of exch. Ca.
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