Quantification of microstructural changes in salorthidic fluvaquents using rheological and particle charge techniques

Salorthidic Fluvaquents originating from Seville, Andalusia, were sampled and subjected to rheological and particle charge investigations. Structural changes in a managed and a natural site under pasture were compared based on physicochemical laboratory analyses, scanning electron microscopy, particle charge density (PCD) measurements, and rheological tests. An uncultivated site located at the riparian zone of the Guadalquivir River showed a natural fluvio-marine-affected development. A regular influx and exchange of salts in the groundwater, especially in the form of NaCl and calcite, dominate soil genetic processes. In contrast, drainage of the saline-sodic soils for cultivation, furrow irrigation, and phosphogypsum fertilization have led to a modification of the salinity gradients throughout the reclaimed soil profile. Sodium ions on the exchangers were released due to the Ca amendment, which led to a decreased exchangeable Na + concentration (exchangeable Na percentage [ESP] < 15) in the topsoil. The soil microstructure of the carbonate-rich and clayey soil remained stable, and surface sealing and crusting were reduced, particularly in the Ap horizon. Results from PCD measurements, derived zeta potential, ζ, and the rheological parameters loss factor tanδ and integral z were consistent. Comparing reclaimed and natural conditions, the rheological parameters integral z and ζ potential showed a linear correlation to ESP and the cation ratio of soil structural stability. This was indicated by increased integral z values and ζ potentials, showing a trend toward stable agglomeration and increased microstructural strength in the case of the ameliorated reclaimed topsoil. Phosphogypsum amelioration was appraisal as successful using approach.

Saved in:
Bibliographic Details
Main Authors: Markgraf, W., Moreno Lucas, Félix, Horn, Rainer
Format: artículo biblioteca
Language:English
Published: Soil Science Society of America 2012
Online Access:http://hdl.handle.net/10261/65687
Tags: Add Tag
No Tags, Be the first to tag this record!
id dig-irnas-es-10261-65687
record_format koha
spelling dig-irnas-es-10261-656872016-02-17T12:10:40Z Quantification of microstructural changes in salorthidic fluvaquents using rheological and particle charge techniques Markgraf, W. Moreno Lucas, Félix Horn, Rainer Salorthidic Fluvaquents originating from Seville, Andalusia, were sampled and subjected to rheological and particle charge investigations. Structural changes in a managed and a natural site under pasture were compared based on physicochemical laboratory analyses, scanning electron microscopy, particle charge density (PCD) measurements, and rheological tests. An uncultivated site located at the riparian zone of the Guadalquivir River showed a natural fluvio-marine-affected development. A regular influx and exchange of salts in the groundwater, especially in the form of NaCl and calcite, dominate soil genetic processes. In contrast, drainage of the saline-sodic soils for cultivation, furrow irrigation, and phosphogypsum fertilization have led to a modification of the salinity gradients throughout the reclaimed soil profile. Sodium ions on the exchangers were released due to the Ca amendment, which led to a decreased exchangeable Na + concentration (exchangeable Na percentage [ESP] < 15) in the topsoil. The soil microstructure of the carbonate-rich and clayey soil remained stable, and surface sealing and crusting were reduced, particularly in the Ap horizon. Results from PCD measurements, derived zeta potential, ζ, and the rheological parameters loss factor tanδ and integral z were consistent. Comparing reclaimed and natural conditions, the rheological parameters integral z and ζ potential showed a linear correlation to ESP and the cation ratio of soil structural stability. This was indicated by increased integral z values and ζ potentials, showing a trend toward stable agglomeration and increased microstructural strength in the case of the ameliorated reclaimed topsoil. Phosphogypsum amelioration was appraisal as successful using approach. Peer Reviewed 2013-02-01T17:06:09Z 2013-02-01T17:06:09Z 2012 2013-02-01T17:06:10Z artículo http://purl.org/coar/resource_type/c_6501 doi: 10.2136/vzj2011.0061 issn: 1539-1663 e-issn: 1539-1663 Vadose Zone Journal 11(1): (2012) http://hdl.handle.net/10261/65687 10.2136/vzj2011.0061 en none Soil Science Society of America
institution IRNAS ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-irnas-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IRNAS España
language English
description Salorthidic Fluvaquents originating from Seville, Andalusia, were sampled and subjected to rheological and particle charge investigations. Structural changes in a managed and a natural site under pasture were compared based on physicochemical laboratory analyses, scanning electron microscopy, particle charge density (PCD) measurements, and rheological tests. An uncultivated site located at the riparian zone of the Guadalquivir River showed a natural fluvio-marine-affected development. A regular influx and exchange of salts in the groundwater, especially in the form of NaCl and calcite, dominate soil genetic processes. In contrast, drainage of the saline-sodic soils for cultivation, furrow irrigation, and phosphogypsum fertilization have led to a modification of the salinity gradients throughout the reclaimed soil profile. Sodium ions on the exchangers were released due to the Ca amendment, which led to a decreased exchangeable Na + concentration (exchangeable Na percentage [ESP] < 15) in the topsoil. The soil microstructure of the carbonate-rich and clayey soil remained stable, and surface sealing and crusting were reduced, particularly in the Ap horizon. Results from PCD measurements, derived zeta potential, ζ, and the rheological parameters loss factor tanδ and integral z were consistent. Comparing reclaimed and natural conditions, the rheological parameters integral z and ζ potential showed a linear correlation to ESP and the cation ratio of soil structural stability. This was indicated by increased integral z values and ζ potentials, showing a trend toward stable agglomeration and increased microstructural strength in the case of the ameliorated reclaimed topsoil. Phosphogypsum amelioration was appraisal as successful using approach.
format artículo
author Markgraf, W.
Moreno Lucas, Félix
Horn, Rainer
spellingShingle Markgraf, W.
Moreno Lucas, Félix
Horn, Rainer
Quantification of microstructural changes in salorthidic fluvaquents using rheological and particle charge techniques
author_facet Markgraf, W.
Moreno Lucas, Félix
Horn, Rainer
author_sort Markgraf, W.
title Quantification of microstructural changes in salorthidic fluvaquents using rheological and particle charge techniques
title_short Quantification of microstructural changes in salorthidic fluvaquents using rheological and particle charge techniques
title_full Quantification of microstructural changes in salorthidic fluvaquents using rheological and particle charge techniques
title_fullStr Quantification of microstructural changes in salorthidic fluvaquents using rheological and particle charge techniques
title_full_unstemmed Quantification of microstructural changes in salorthidic fluvaquents using rheological and particle charge techniques
title_sort quantification of microstructural changes in salorthidic fluvaquents using rheological and particle charge techniques
publisher Soil Science Society of America
publishDate 2012
url http://hdl.handle.net/10261/65687
work_keys_str_mv AT markgrafw quantificationofmicrostructuralchangesinsalorthidicfluvaquentsusingrheologicalandparticlechargetechniques
AT morenolucasfelix quantificationofmicrostructuralchangesinsalorthidicfluvaquentsusingrheologicalandparticlechargetechniques
AT hornrainer quantificationofmicrostructuralchangesinsalorthidicfluvaquentsusingrheologicalandparticlechargetechniques
_version_ 1777664540699262976