Details
| Original language | English |
|---|---|
| Pages (from-to) | 230-250 |
| Number of pages | 21 |
| Journal | GEODERMA |
| Volume | 129 |
| Issue number | 3-4 |
| Publication status | Published - Dec 2005 |
Abstract
Occurrence of gypsum in soils from loess of the Central-German Chernozem region indicates that local climatic conditions with low precipitation (average <500 mm a-1) and a real evaporation between 450 and 460 mm do not allow leaching of weakly soluble gypsum from soils. At a site close to the strip mine Etzdorf, gypsum is accumulated in the Ck-horizon of a Haplic Chernozem down to a depth of about 1.5 m, its distribution being nonuniform. Calculated total gypsum in the Haplic Chernozem amounts from 10-20 t ha-1. The highest accumulation of gypsum, obviously by solution transport and evaporation, can be observed in a profile exposed to the air since about 1960. In this profile maximum, SO42- values, however, are not found on the surface of the outermost aggregates with whitish efflorescence, but at 20 cm depth in the profile. In a Eutric Podzoluvisol, the precipitation of gypsum developed on living roots as well as in pores of former roots. In a buried Chernozem, large euhedral gypsum crystals with a diameter of up to 1.5 cm were found. Gypsum crystals occur in different shapes and sizes such as euhedral lenticular, rosette-like, and equigranular ones. Even soils having undergone leaching processes reveal unusual increases of SO42- at 40-50 cm depth. This may be an indicator of more recent SO4 2- input due to atmospheric deposition since the beginning of industrialization. It is supposed that gypsum is formed by the reaction of atmogenic sulfuric acid with different Ca sources in the soil.
Keywords
- Atmospheric S deposition, Central-German Chernozem region, Gypsum content, Micromorphology, Soils
ASJC Scopus subject areas
- Agricultural and Biological Sciences(all)
- Soil Science
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In: GEODERMA, Vol. 129, No. 3-4, 12.2005, p. 230-250.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Occurrence, formation, and micromorphology of gypsum in soils from the Central-German Chernozem region
AU - Dultz, Stefan
AU - Kühn, Peter
N1 - Copyright: Copyright 2008 Elsevier B.V., All rights reserved.
PY - 2005/12
Y1 - 2005/12
N2 - Occurrence of gypsum in soils from loess of the Central-German Chernozem region indicates that local climatic conditions with low precipitation (average <500 mm a-1) and a real evaporation between 450 and 460 mm do not allow leaching of weakly soluble gypsum from soils. At a site close to the strip mine Etzdorf, gypsum is accumulated in the Ck-horizon of a Haplic Chernozem down to a depth of about 1.5 m, its distribution being nonuniform. Calculated total gypsum in the Haplic Chernozem amounts from 10-20 t ha-1. The highest accumulation of gypsum, obviously by solution transport and evaporation, can be observed in a profile exposed to the air since about 1960. In this profile maximum, SO42- values, however, are not found on the surface of the outermost aggregates with whitish efflorescence, but at 20 cm depth in the profile. In a Eutric Podzoluvisol, the precipitation of gypsum developed on living roots as well as in pores of former roots. In a buried Chernozem, large euhedral gypsum crystals with a diameter of up to 1.5 cm were found. Gypsum crystals occur in different shapes and sizes such as euhedral lenticular, rosette-like, and equigranular ones. Even soils having undergone leaching processes reveal unusual increases of SO42- at 40-50 cm depth. This may be an indicator of more recent SO4 2- input due to atmospheric deposition since the beginning of industrialization. It is supposed that gypsum is formed by the reaction of atmogenic sulfuric acid with different Ca sources in the soil.
AB - Occurrence of gypsum in soils from loess of the Central-German Chernozem region indicates that local climatic conditions with low precipitation (average <500 mm a-1) and a real evaporation between 450 and 460 mm do not allow leaching of weakly soluble gypsum from soils. At a site close to the strip mine Etzdorf, gypsum is accumulated in the Ck-horizon of a Haplic Chernozem down to a depth of about 1.5 m, its distribution being nonuniform. Calculated total gypsum in the Haplic Chernozem amounts from 10-20 t ha-1. The highest accumulation of gypsum, obviously by solution transport and evaporation, can be observed in a profile exposed to the air since about 1960. In this profile maximum, SO42- values, however, are not found on the surface of the outermost aggregates with whitish efflorescence, but at 20 cm depth in the profile. In a Eutric Podzoluvisol, the precipitation of gypsum developed on living roots as well as in pores of former roots. In a buried Chernozem, large euhedral gypsum crystals with a diameter of up to 1.5 cm were found. Gypsum crystals occur in different shapes and sizes such as euhedral lenticular, rosette-like, and equigranular ones. Even soils having undergone leaching processes reveal unusual increases of SO42- at 40-50 cm depth. This may be an indicator of more recent SO4 2- input due to atmospheric deposition since the beginning of industrialization. It is supposed that gypsum is formed by the reaction of atmogenic sulfuric acid with different Ca sources in the soil.
KW - Atmospheric S deposition
KW - Central-German Chernozem region
KW - Gypsum content
KW - Micromorphology
KW - Soils
UR - http://www.scopus.com/inward/record.url?scp=27644510935&partnerID=8YFLogxK
U2 - 10.1016/j.geoderma.2005.01.022
DO - 10.1016/j.geoderma.2005.01.022
M3 - Article
AN - SCOPUS:27644510935
VL - 129
SP - 230
EP - 250
JO - GEODERMA
JF - GEODERMA
SN - 0016-7061
IS - 3-4
ER -