AbstractA pH‐stat procedure was previously developed to determine the effective particle‐size distribution of soil carbonates. The results obtained by the pH‐stat procedure are influenced by the accessibility of carbonate surface sites to the titrant and, therefore, provide a methodology for the comparison of carbonate dispersion treatments. In this study, the influence of dispersion treatment on the determination of effective particle‐size distribution of soil carbonates was examined. The treatments consisted of agitation, sonication, or Na saturation of clay cation‐exchange sites of calcareous soils representing three series (Austin: fine‐silty, carbonatic, thermic Entic Haplustoll; Rio Grande: coarse‐silty, mixed (calcareous), hyperthermic Typic Ustifluvent; Victoria: fine, montmorillonitic, hyperthermic Udic Pellustert). Shaking and sonication pretreatments resulted in increases in the experimentally determined proportion of effective fine‐clay size soil carbonates and corresponding decreases in the effective silt‐ and sand‐size carbonates, when compared with the untreated soils. As the intensity of either of these pretreatments was increased, the proportion of effective clay‐size carbonates increased. Scanning electron microscopy indicated that the longer and more intense sonication treatments resulted in a higher degree of disruption or grinding of carbonate aggregates. Sodium saturation of the clay cation‐exchange sites resulted in the most effective disaggregation of the phyllosilicate‐carbonate complex, as indicated by the greatest proportion of effective clay‐size and lowest proportions of effective silt‐ and sand‐size carbonates. Sodium saturation may also result in a lower degree of disruption of carbonate particles or carbonate‐cemented aggregates than may occur with intense sonication. An initial Na saturation is, therefore, recommended as a pretreatment for the determination of effective particle‐size distribution of soil carbonates.
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