Earth: An Introduction to Physical Geology (12th Edition)

Published by Pearson
ISBN 10: 0134074254
ISBN 13: 978-0-13407-425-2

Chapter 6 - Section 6.3 - Chemical Weathering - Concept Checks - Page 192: 3

Answer

When carbonic acid (H2CO3) reacts with potassium feldspar (KAlSi3O8), a common mineral in the group of feldspar minerals, the following reaction can occur: KAlSi3O8 + 2H2CO3 → Al2Si2O5(OH)4 + K+ + 2HCO3- In this reaction, carbonic acid reacts with potassium feldspar to produce kaolinite (Al2Si2O5(OH)4), potassium ions (K+), and bicarbonate ions (HCO3-). Kaolinite is a clay mineral that forms as a result of the weathering and alteration of potassium feldspar. The reaction with carbonic acid causes the breakdown of potassium feldspar, releasing potassium ions and forming kaolinite as a weathering product. The bicarbonate ions are dissolved in water and may be transported away from the reaction site. It's important to note that the reaction of carbonic acid with potassium feldspar may vary depending on the specific conditions, concentrations, and presence of other compounds. However, the general process involves the dissolution and alteration of potassium feldspar into different minerals through chemical weathering.

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