Dynamics of soil water content in the rhizosphere

Water flow from soil to plants depends on the properties of the soil next to roots, the rhizosphere. Although several studies showed that the rhizosphere has different properties than the bulk soil, effects of the rhizosphere on root water uptake are commonly neglected. To investigate the rhizospher...

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Published inPlant and soil Vol. 332; no. 1-2; pp. 163 - 176
Main Authors Carminati, Andrea, Moradi, Ahmad B, Vetterlein, Doris, Vontobel, Peter, Lehmann, Eberhard, Weller, Ulrich, Vogel, Hans-Jörg, Oswald, Sascha E
Format Journal Article
LanguageEnglish
Published Dordrecht Dordrecht : Springer Netherlands 01.07.2010
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Springer Nature B.V
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Abstract Water flow from soil to plants depends on the properties of the soil next to roots, the rhizosphere. Although several studies showed that the rhizosphere has different properties than the bulk soil, effects of the rhizosphere on root water uptake are commonly neglected. To investigate the rhizosphere's properties we used neutron radiography to image water content distributions in soil samples planted with lupins during drying and subsequent rewetting. During drying, the water content in the rhizosphere was 0.05 larger than in the bulk soil. Immediately after rewetting, the picture reversed and the rhizosphere remained markedly dry. During the following days the water content of the rhizosphere increased and after 60 h it exceeded that of the bulk soil. The rhizosphere's thickness was approximately 1.5 mm. Based on the observed dynamics, we derived the distinct, hysteretic and time-dependent water retention curve of the rhizosphere. Our hypothesis is that the rhizosphere's water retention curve was determined by mucilage exuded by roots. The rhizosphere properties reduce water depletion around roots and weaken the drop of water potential towards roots, therefore favoring water uptake under dry conditions, as demonstrated by means of analytical calculation of water flow to a single root.
AbstractList Water flow from soil to plants depends on the properties of the soil next to roots, the rhizosphere. Although several studies showed that the rhizosphere has different properties than the bulk soil, effects of the rhizosphere on root water uptake are commonly neglected. To investigate the rhizosphere's properties we used neutron radiography to image water content distributions in soil samples planted with lupins during drying and subsequent rewetting. During drying, the water content in the rhizosphere was 0.05 larger than in the bulk soil. Immediately after rewetting, the picture reversed and the rhizosphere remained markedly dry. During the following days the water content of the rhizosphere increased and after 60 h it exceeded that of the bulk soil. The rhizosphere's thickness was approximately 1.5 mm. Based on the observed dynamics, we derived the distinct, hysteretic and time-dependent water retention curve of the rhizosphere. Our hypothesis is that the rhizosphere's water retention curve was determined by mucilage exuded by roots. The rhizosphere properties reduce water depletion around roots and weaken the drop of water potential towards roots, therefore favoring water uptake under dry conditions, as demonstrated by means of analytical calculation of water flow to a single root. [PUBLICATION ABSTRACT]
Water flow from soil to plants depends on the properties of the soil next to roots, the rhizosphere. Although several studies showed that the rhizosphere has different properties than the bulk soil, effects of the rhizosphere on root water uptake are commonly neglected. To investigate the rhizosphere’s properties we used neutron radiography to image water content distributions in soil samples planted with lupins during drying and subsequent rewetting. During drying, the water content in the rhizosphere was 0.05 larger than in the bulk soil. Immediately after rewetting, the picture reversed and the rhizosphere remained markedly dry. During the following days the water content of the rhizosphere increased and after 60 h it exceeded that of the bulk soil. The rhizosphere’s thickness was approximately 1.5 mm. Based on the observed dynamics, we derived the distinct, hysteretic and time-dependent water retention curve of the rhizosphere. Our hypothesis is that the rhizosphere’s water retention curve was determined by mucilage exuded by roots. The rhizosphere properties reduce water depletion around roots and weaken the drop of water potential towards roots, therefore favoring water uptake under dry conditions, as demonstrated by means of analytical calculation of water flow to a single root.
Water flow from soil to plants depends on the properties of the soil next to roots, the rhizosphere. Although several studies showed that the rhizosphere has different properties than the bulk soil, effects of the rhizosphere on root water uptake are commonly neglected. To investigate the rhizosphere's properties we used neutron radiography to image water content distributions in soil samples planted with lupins during drying and subsequent rewetting. During drying, the water content in the rhizosphere was 0.05 larger than in the bulk soil. Immediately after rewetting, the picture reversed and the rhizosphere remained markedly dry. During the following days the water content of the rhizosphere increased and after 60 h it exceeded that of the bulk soil. The rhizosphere's thickness was approximately 1.5 mm. Based on the observed dynamics, we derived the distinct, hysteretic and time-dependent water retention curve of the rhizosphere. Our hypothesis is that the rhizosphere's water retention curve was determined by mucilage exuded by roots. The rhizosphere properties reduce water depletion around roots and weaken the drop of water potential towards roots, therefore favoring water uptake under dry conditions, as demonstrated by means of analytical calculation of water flow to a single root.
Water flow from soil to plants depends on the properties of the soil next to roots, the rhizosphere. Although several studies showed that the rhizosphere has different properties than the bulk soil, effects of the rhizosphere on root water uptake are commonly neglected. To investigate the rhizosphere's properties we used neutron radiography to image water content distributions in soil samples planted with lupins during drying and subsequent rewetting. During drying, the water content in the rhizosphere was 0.05 larger than in the bulk soil. Immediately after rewetting, the picture reversed and the rhizosphere remained markedly dry. During the following days the water content of the rhizosphere increased and after 60 h it exceeded that of the bulk soil. The rhizosphere's thickness was approximately 1.5 mm. Based on the observed dynamics, we derived the distinct, hysteretic and time-dependent water retention curve of the rhizosphere. Our hypothesis is that the rhizosphere's water retention curve was determined by mucilage exuded by roots. The rhizosphere properties reduce water depletion around roots and weaken the drop of water potential towards roots, therefore favoring water uptake under dry conditions, as demonstrated by means of analytical calculation of water flow to a single root. Keywords Root water uptake * Water retention curve * Rhizosphere * Neutron radiography * Mucilage * Hysteresis
Audience Academic
Author Lehmann, Eberhard
Carminati, Andrea
Moradi, Ahmad B.
Vontobel, Peter
Vogel, Hans-Jörg
Weller, Ulrich
Vetterlein, Doris
Oswald, Sascha E.
Author_xml – sequence: 1
  fullname: Carminati, Andrea
– sequence: 2
  fullname: Moradi, Ahmad B
– sequence: 3
  fullname: Vetterlein, Doris
– sequence: 4
  fullname: Vontobel, Peter
– sequence: 5
  fullname: Lehmann, Eberhard
– sequence: 6
  fullname: Weller, Ulrich
– sequence: 7
  fullname: Vogel, Hans-Jörg
– sequence: 8
  fullname: Oswald, Sascha E
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Fri Feb 02 04:09:31 EST 2024
Thu Sep 12 16:58:11 EDT 2024
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IsPeerReviewed true
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Issue 1-2
Keywords Neutron radiography
Rhizosphere
Root water uptake
Water retention curve
Mucilage
Hysteresis
Dynamic characteristic
Root
Nuclear method
Soil moisture
Property of soil
Physical properties
Soil water properties
Vegetative apparatus
Water absorption
Soil plant relation
Water holding capacity
Physical method
Language English
License CC BY 4.0
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Notes http://dx.doi.org/10.1007/s11104-010-0283-8
PQID 375542592
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springer_journals_10_1007_s11104_010_0283_8
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PublicationCentury 2000
PublicationDate 2010-07-01
PublicationDateYYYYMMDD 2010-07-01
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  year: 2010
  text: 2010-07-01
  day: 01
PublicationDecade 2010
PublicationPlace Dordrecht
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PublicationSubtitle An International Journal on Plant-Soil Relationships
PublicationTitle Plant and soil
PublicationTitleAbbrev Plant Soil
PublicationYear 2010
Publisher Dordrecht : Springer Netherlands
Springer
Springer Netherlands
Springer Nature B.V
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Snippet Water flow from soil to plants depends on the properties of the soil next to roots, the rhizosphere. Although several studies showed that the rhizosphere has...
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SubjectTerms Agronomy. Soil science and plant productions
Animal, plant and microbial ecology
Biological and medical sciences
Biomedical and Life Sciences
Biophysics
Botany
Drying
Ecology
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Hydraulic measurements
hysteresis
Life Sciences
Moisture
Moisture content
Mucilage
Neutron radiography
Physical properties
Physics, chemistry, biochemistry and biology of agricultural and forest soils
Plant Physiology
Plant roots
Plant Sciences
Plants
Radiography
Regular Article
Retention
Rhizosphere
Root water uptake
Roots
Samples
Sand soils
Soil dynamics
Soil hydraulic properties
Soil moisture
Soil properties
Soil science
Soil Science & Conservation
Soil sciences
Soil water
Soil water content
Soil water retention
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Water
Water and solute dynamics
Water content
Water flow
Water potential
Water retention curve
Water uptake
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Title Dynamics of soil water content in the rhizosphere
URI https://www.jstor.org/stable/24130139
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