Sentence examples for sorption maximum from inspiring English sources

In the case of HMO, % C desorption is lower for a C loading significantly below the sorption maximum compared to % C desorption at C loadings at or near the sorption maximum (Fig. 6).

The lesser reactivity and surface area of goethite compared to 2-line ferrihydrite is the most likely reason for the observed disparity in sorption maximum.

Compared with CF, SM and RS increased the Langmuir P sorption maximum (Smax) of the paddy soil by 30 and 10%, respectively (p < 0.05).

The observed sorption maximum is mostly consistent with what Chen et al. observed at pH 7, although our experiments resulted in approximately 10% higher sorption relative to a system without exogenous calcium [14].

TCE sorption onto an iron surface, as quantified by the Langmuir sorption maximum, followed the trend H2-reduced Fe0>HCl-washed Fe0>untreated Fe0.887887, 0.365 and 0.311 mg/g, respectively).

This study was conducted to assess various P sorption indices (PSI) to indicate P sorption maximum (Qmax) of soils, and their derived DPS indices as indicators of dissolved reactive P (DRP) concentration in soil leachate.

Sorption, however, will likely be low due to low P sorption maxima and low binding energies.

The SSA-normalized DOM sorption maxima for HMO and goethite are 6.4 × 102 and 4.8 × 102 μg C m−2, respectively (Fig. 6).

Phosphorus binding energy (K) (0.34 0.60 L/mg) and P sorption maxima (17.8 26.6 L/mg) were low, with very little variation in space and time.

Langmuir isotherm sorption maxima for oxyanions measured in batch experiments were in the following order: perchlorate >> chromate > selenate, consistent with their selectivity.

Sorption parameters (maximum sorption capacity, Qmax and binding coefficient, k) calculated by fitting sorption data to the Langmuir equation showed that Qmax of A and B horizons was very similar for all compounds.