Sentence examples for between calcite and solution from inspiring English sources

Calcium isotope fractionation between calcite and solution is expressed as Δ44/40Cacalcite-aq Δ44/40Cacalcite-aq  − δ44/40Caaq, where δ44/40Cacalcite and δ44/40Caaq are the Ca isotope composition of calcite and the growth solution, respectively.

In this study, the Sr/Ca fractionation between calcite and solution is expressed as a Sr distribution coefficient according to the equation (1) D Sr = [ Sr ] [ Ca ] calcite [ Sr ] [ Ca ] aq where ([Sr]/[Ca] calcite is the molar Sr/Ca ratio of precipitated calcite and ([Sr]/[Ca])aq is the molar Sr/Ca ratio of the growth solution.

Nehrke et al. [20] also investigated the dependence of Sr2+ partitioning between calcite and the parent solution on calcite growth kinetics and the ion ratio and reported that Sr partitioning increases with increasing rates of precipitation.

This is especially true when dealing with interactions between calcite and Cd2+(aq), since this ion is known to substitute for Ca2+ in the calcite structure [12].

The difference in friction between calcite and Ot-1 was small (≈10%) as well as the difference between Ot-1 and Ot-2.

At 25 °C the calcium isotope fractionation between calcite and aqueous calcium ions (Δ44/40Cacalcite-aq Δ44/40Cacalcite-aq− δ44/40Caaq) correlates inversely to log  R values for all experiments.

In suspensions maintained at constant composition by replenishing components lost during precipitation, the distribution coefficient of Sr2+ or other co-precipitating metals between the calcite and the parent solution are determined by the Henderson-Karcek distribution coefficient equation [12]: D P S r 2 + = X P S r 2 +  / X P C a 2 +  M S S r 2 +  / M S C a 2 +  (4).

When Δ44/40Cacalcite-aq Δ44/40Cacalcite-aq different ionic strengths are plotted as a function of precipitation rate (Fig. 3 ), it is obvaluesthat precipitation rate is the primeasuredtor that controls Ca isotope fractionation between precipitatedifferent and the growth solutionic

In the first, mixtures of Na-montmorillonite, magnetite, native Fe, calcite, and NaCl solutions were reacted at 250 °C, Psat for between 93 and 114 days.

Discussing scale formation and fragmentation, two interfaces are considered to be of crucial importance: (i) the interface between calcite scale and the sulfide corrosion products and (ii) the interface between thermal fluid and calcite scale.

Systematic correlation between calcite dissolution and the resulting creep strain is consistently demonstrated by all the different chalk types.