Table 2 Average chemical composition variation of evaporitic samples before and after slaking with distilled water and groundwater.

From: Effects of groundwater and distilled water on the durability of evaporitic rocks

 

wt. (%)

CaO

SO3

Na2O

MgO

Al2O3

SiO2

P2O5

K2O

Fe2O3

TiO2

Ti

Cl

Mn

Sr

Ba

Zr

Slaking fluid

Before slaking

47.494

50.074

0.25

0.844

0.164

0.613

0.023

0.051

0.122

0.024

0.015

0.240

0.001

0.088

0.019

0.013

Distilled water

After slaking

46.519

51.835

0.466

0.643

0.108

0.106

0.036

0.014

0.036

0.001

0.001

0.078

0.000

0.114

0.015

0.001

 

Differences

0.975

−1.761

−0.216

0.201

0.056

0.507

−0.013

0.037

0.086

0.023

0.014

0.161

0.001

−0.026

0.004

0.012

Groundwater*

After slaking

39.801

42.523

0.673

0.707

0.076

0.121

0.021

0.122

0.039

0.001

0.001

3.220

0.000

0.144

0.017

0.001

 

Differences

7.693

7.755

−0.423

0.137

0.088

0.492

0.002

−0.071

0.083

0.023

0.014

−2.980

0.001

−0.056

0.002

0.012

Total samples = 14–16**

                 
  1. *Groundwater specification: Groundwater level = 10–40 m, Temperature = 21.5–31.2 (\(^\circ \)C), Salinity = 20,000–65,000 (ppm), pH = 7.14–9.45, TDS = 32,700–175,360 (ppm), EC = 28,100–274,000 (μ mhos/cm).
  2. **Chemical composition of two samples were missing in case of groundwater as a slaking fluid.