Dynamics of sulfate and basic cations in soil solution as affected by gypsum fertilization in an Ultisol of Southern Brazil

The objective of this study was to evaluate the short-term dynamics of chemical species of sulfate and the main basic cations in the soil solution affected by the application of different sulfur (S) rates using agricultural gypsum. The experiment was carried out in an Ultisol with 14% clay, managed...

Full description

Saved in:
Bibliographic Details
Published in:Archiv für Acker- und Pflanzenbau und Bodenkunde 2019-12, Vol.65 (14), p.1998-2012
Main Authors: Tiecher, Tales, Denardin, Luiz Gustavo De Oliveira, Martins, Amanda Posselt, Pias, Osmar Henrique, Nunes, Leonardo Rodrigues, Tiecher, Tadeu Luis, Alvarez, Jimmy Walter Rasche, Mallmann, Fábio Joel Kochem, Brunetto, Gustavo, Rheinheimer Dos Santos, Danilo
Format: Article
Language:English
Subjects:
Agricultural management
Calcium
Cation exchange
Cation exchanging
cation leaching
Cations
Chemical speciation
Fertilization
Gypsum
Lysimeters
Magnesium
no-tillage
Organic chemistry
Sandy soils
Soil dynamics
Soil fertility
Soil profiles
Soil properties
Soil solution
Sulfates
Sulfur
Tillage
Ultisol
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:The objective of this study was to evaluate the short-term dynamics of chemical species of sulfate and the main basic cations in the soil solution affected by the application of different sulfur (S) rates using agricultural gypsum. The experiment was carried out in an Ultisol with 14% clay, managed under no-tillage for 14 yrs in Southern Brazil. Four rates of S (0, 5, 10 and 20 kg of S ha −1 ) were evaluated using agricultural gypsum (CaSO 4 ) as S-source. The soil solution was collected using porous capsule lysimeters before and at 9, 17, 37, 60, 76 and 109 d after the gypsum application, at depths of 20 and 60 cm. Surface application of gypsum rapidly increases the sulfate concentration in the soil solution at 20 cm depth. However, in less than 30 d, the effect of the S rates on the soil solution at 20 cm was minimal, with an increase in sulfate concentration in the soil solution at 60 cm depth after 17 d. Sulfated fertilization via agricultural gypsum at rates greater than 10 kg ha −1 in sandy soil with low cation exchange capacity increased the mobility of Ca and Mg in the soil profile.
ISSN:0365-0340
1476-3567
DOI:10.1080/03650340.2019.1587748