Mobile soil colloids play an important role in affecting soil hydraulic properties and soil formation, as well as in facilitating the transport of strongly sorbing constituents (e.g., contaminants, pesticides, nutrients) in subsurface environments. Accurate quantification of mobile colloids is thus essential for understanding and prediction of soil element migration, changes in soil hydraulic properties, and colloid-associated contaminants in natural and managed systems. However, quantification of colloids in field samples, especially the <0.45-μm fractions, which are traditionally considered dissolved solutes, has largely been hindered due to the lack of reliable methods. In this study, we developed a simple and efficient methodology of using size-dependent correlations between nephelometric turbidity and mass concentrations of colloids for quantifying colloids in the <0.1-, 0.1- to 0.45-, and 0.45- to 1.0-μm fractions. The correlations were measured using model colloids (latex, silica, and Fe oxide particles) and soil colloids extracted from 37 soils. We found that colloid size strongly affected concentration–turbidity relationships, while colloid composition played a less important role in shifting the correlations. The size-dependent concentration–turbidity correlations were further tested against gravimetric measurements using additional field samples and found to be more accurate than correlations that do not consider size effects. The relatively insignificant particle composition effect indicates the practically “universal” applicability of the reported correlations. In addition, the correlations, for the first time, allow quantification of colloids in different size fractions in environmental samples. This would enhance our capability to more accurately quantify the colloidal pools in natural systems, which have strong implications for understanding the processes and mechanisms of colloid and colloid-associated-constituent mobilization and transport.
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Research Article|
May 01, 2017
Size-Dependent Turbidimetric Quantification of Suspended Soil Colloids
Jing Yan;
Jing Yan
a
Dep. of Plant and Soil Sciences, Univ. of Delaware, Newark, DE 19716
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Xia Meng;
Xia Meng
b
Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, No. 88 Xuefulu, Kunming, Yunnan 650223, China
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Yan Jin
a
Dep. of Plant and Soil Sciences, Univ. of Delaware, Newark, DE 19716*
Corresponding author ([email protected]).
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Jing Yan
a
Dep. of Plant and Soil Sciences, Univ. of Delaware, Newark, DE 19716
Xia Meng
b
Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, No. 88 Xuefulu, Kunming, Yunnan 650223, China*
Corresponding author ([email protected]).
Publisher: Soil Science Society of America
Received:
18 Oct 2016
Accepted:
08 Mar 2017
First Online:
03 Jan 2018
Copyright © by the Soil Science Society of America, Inc.
Vadose Zone Journal (2017) 16 (5): 1–8.
Article history
Received:
18 Oct 2016
Accepted:
08 Mar 2017
First Online:
03 Jan 2018
Citation
Jing Yan, Xia Meng, Yan Jin; Size-Dependent Turbidimetric Quantification of Suspended Soil Colloids. Vadose Zone Journal 2017;; 16 (5): 1–8. doi: https://doi.org/10.2136/vzj2016.10.0098
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Index Terms/Descriptors
- aqueous solutions
- Atlantic Coastal Plain
- carbon
- colloidal materials
- concentration
- Delaware
- Denmark
- Europe
- field studies
- goethite
- grain size
- hematite
- iron
- measurement
- metals
- New Castle County Delaware
- organic carbon
- oxides
- particles
- pore water
- quantitative analysis
- Scandinavia
- size
- size distribution
- soils
- suspended materials
- transport
- turbidity
- United States
- unsaturated zone
- Western Europe
- turbidimetric method
- Blackbird State Forest
Latitude & Longitude
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