Sentence examples for dissolution of limestone from inspiring English sources

As previously noted, the largest and most common caves are those formed by dissolution of limestone or dolomite.

The caves were formed by the dissolution of limestone by water, which also produced striking stalactite and stalagmite rock formations.

Kinetic analysis of the results indicates that the dissolution of limestone is according to the shrinking core model with surface control, i.e. 1−(1−3)1/3 = kt.

The caves were formed by the dissolution of limestone by water, a continuing process; their natural temperature is 54 °F (12 °C), with a relative humidity of a high 87 percent.

In the present work, the dissolution of limestone from different sources in South Africa has been studied in a pH-Stat apparatus under conditions similar to those encountered in wet FGD processes.

In the Yucatan, cenotes or water sinkholes formed by the dissolution of limestone and surrounded with a characteristic dense layer of heterogeneous vegetation, are the main sources of water for plant and animal assemblages.

Elevated Ca concentrations may be attributed to dissolution of limestones, Ca-rich feldspars, and potentially due to biodegradation or organic matter in upper soil horizons.

In this study the dissolution rate of limestone has been modeled with the flux equations, including the electrical potential gradient and assuming that the electrical potential gradient is zero.

For the complete development of an underground drainage system, it is necessary that the water-carrying conduits also flush out the soil that washes in through sinkholes, the sediment load of sinking streams, and the insoluble weathering products from the dissolution of the limestone.

Such finding reflects the interaction between water and aquifer rocks causing dissolution of carbonates (limestone and dolomite) under acidic pH conditions (pH of rainwater).

Based on the water rock interaction types, Piper triplot (Piper 1944; Fig. 8a) classified tap waters and the majority of borewell waters as Ca HCO3 or Ca Mg HCO3 type, consistent with dissolution of dolomitic limestone and silicate (i.e., amphiboles, pyroxenes, olivine and biotite) minerals.