Surface charge and zero-charge points

J. Chorover

doi:10.1016/B978-0-12-822974-3.00148-8

Surface charge and zero-charge points

J. Chorover

Research output: Chapter in Book/Report/Conference proceeding › Chapter

1 Scopus citations

Abstract

Soil surface charge exerts strong control over the adsorption of ions from the soil solution, colloidal stability and particle aggregation, and rates of mineral dissolution. There are multiple methods for quantifying surface charge including proton titrations and measurements of surface excess of charged ions. These methods can be used to determine the pH values where one or more components of surface charge vanishes (i.e., points of zero charge).

Original language	English (US)
Title of host publication	Encyclopedia of Soils in the Environment, Second Edition
Publisher	Elsevier
Pages	V2-368-V2-375
ISBN (Electronic)	9780128229743
DOIs	https://doi.org/10.1016/B978-0-12-822974-3.00148-8
State	Published - Jan 1 2023

Keywords

Ion adsorption
Natural particles
pH dependent charge
Points of zero charge
Soil surface chemistry
Structural charge
Surface charge

ASJC Scopus subject areas

General Engineering
General Agricultural and Biological Sciences

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10.1016/B978-0-12-822974-3.00148-8

Cite this

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title = "Surface charge and zero-charge points",

abstract = "Soil surface charge exerts strong control over the adsorption of ions from the soil solution, colloidal stability and particle aggregation, and rates of mineral dissolution. There are multiple methods for quantifying surface charge including proton titrations and measurements of surface excess of charged ions. These methods can be used to determine the pH values where one or more components of surface charge vanishes (i.e., points of zero charge).",

keywords = "Ion adsorption, Natural particles, pH dependent charge, Points of zero charge, Soil surface chemistry, Structural charge, Surface charge",

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AB - Soil surface charge exerts strong control over the adsorption of ions from the soil solution, colloidal stability and particle aggregation, and rates of mineral dissolution. There are multiple methods for quantifying surface charge including proton titrations and measurements of surface excess of charged ions. These methods can be used to determine the pH values where one or more components of surface charge vanishes (i.e., points of zero charge).

KW - Ion adsorption

KW - Natural particles

KW - pH dependent charge

KW - Points of zero charge

KW - Soil surface chemistry

KW - Structural charge

KW - Surface charge

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M3 - Chapter

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SP - V2-368-V2-375

BT - Encyclopedia of Soils in the Environment, Second Edition

PB - Elsevier

ER -

Surface charge and zero-charge points

Abstract

Keywords

ASJC Scopus subject areas

Access to Document

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