Soil strength and macropore volume limit root elongation rates in many UK agricultural soils

Tracy A. Valentine*, Paul D. Hallett, Kirsty Binnie, Mark W. Young, Geoffrey R. Squire, Cathy Hawes, A. Glyn Bengough

*Corresponding author for this work

Research output: Contribution to journalArticle

69 Citations (Scopus)

Abstract

Background and Aims Simple indicators of crop and cultivar performance across a range of soil types and management are needed for designing and testing sustainable cropping practices. This paper determined the extent to which soil chemical and physical properties, particularly soil strength and pore-size distribution influences root elongation in a wide range of agricultural top soils, using a seedling-based indicator. Methods Intact soil cores were sampled from the topsoil of 59 agricultural fields in Scotland, representing a wide geographic spread, range of textures and management practices. Water release characteristics, dry bulk density and needle penetrometer resistance were measured on three cores from each field. Soil samples from the same locations were sieved, analysed for chemical characteristics, and packed to dry bulk density of 1·0 g cm−3 to minimize physical constraints. Root elongation rates were determined for barley seedlings planted in both intact field and packed soil cores at a water content close to field capacity (–20 kPa matric potential). Key Results Root elongation in field soil was typically less than half of that in packed soils. Penetrometer resistance was typically between 1 and 3 MPa for field soils, indicating the soils were relatively hard, despite their moderately wet condition (compared with <0·2 MPa for packed soil). Root elongation was strongly linked to differences in physical rather than chemical properties. In field soil root elongation was related most closely to the volume of soil pores between 60 µm and 300 µm equivalent diameter, as estimated from water-release characteristics, accounting for 65·7 % of the variation in the elongation rates. Conclusions Root elongation rate in the majority of field soils was slower than half of the unimpeded (packed) rate. Such major reductions in root elongation rates will decrease rooting volumes and limit crop growth in soils where nutrients and water are scarce.
Original languageEnglish
Pages (from-to)259-270
Number of pages12
JournalAnnals of Botany
Volume110
Issue number2
Early online date8 Jun 2012
DOIs
Publication statusPublished - Jul 2012

Keywords

  • Hordeum vulgare
  • penetration resistance
  • pore diameter
  • bulk density
  • soil chemistry
  • Hordeum-vulgare-L
  • root elongation
  • soil strength
  • moisture availability
  • physical conditions
  • Scotland
  • dry bulk density
  • seminal roots
  • barley
  • mechanical impedance
  • soil porosity
  • wheat triticum-aestivum
  • growth
  • macroporosity
  • water-stress
  • abiotic stress

Cite this

Soil strength and macropore volume limit root elongation rates in many UK agricultural soils. / Valentine, Tracy A.; Hallett, Paul D.; Binnie, Kirsty; Young, Mark W.; Squire, Geoffrey R.; Hawes, Cathy; Bengough, A. Glyn.

In: Annals of Botany, Vol. 110, No. 2, 07.2012, p. 259-270.

Research output: Contribution to journalArticle

Valentine, Tracy A. ; Hallett, Paul D. ; Binnie, Kirsty ; Young, Mark W. ; Squire, Geoffrey R. ; Hawes, Cathy ; Bengough, A. Glyn. / Soil strength and macropore volume limit root elongation rates in many UK agricultural soils. In: Annals of Botany. 2012 ; Vol. 110, No. 2. pp. 259-270.
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title = "Soil strength and macropore volume limit root elongation rates in many UK agricultural soils",
abstract = "Background and Aims Simple indicators of crop and cultivar performance across a range of soil types and management are needed for designing and testing sustainable cropping practices. This paper determined the extent to which soil chemical and physical properties, particularly soil strength and pore-size distribution influences root elongation in a wide range of agricultural top soils, using a seedling-based indicator. Methods Intact soil cores were sampled from the topsoil of 59 agricultural fields in Scotland, representing a wide geographic spread, range of textures and management practices. Water release characteristics, dry bulk density and needle penetrometer resistance were measured on three cores from each field. Soil samples from the same locations were sieved, analysed for chemical characteristics, and packed to dry bulk density of 1·0 g cm−3 to minimize physical constraints. Root elongation rates were determined for barley seedlings planted in both intact field and packed soil cores at a water content close to field capacity (–20 kPa matric potential). Key Results Root elongation in field soil was typically less than half of that in packed soils. Penetrometer resistance was typically between 1 and 3 MPa for field soils, indicating the soils were relatively hard, despite their moderately wet condition (compared with <0·2 MPa for packed soil). Root elongation was strongly linked to differences in physical rather than chemical properties. In field soil root elongation was related most closely to the volume of soil pores between 60 µm and 300 µm equivalent diameter, as estimated from water-release characteristics, accounting for 65·7 {\%} of the variation in the elongation rates. Conclusions Root elongation rate in the majority of field soils was slower than half of the unimpeded (packed) rate. Such major reductions in root elongation rates will decrease rooting volumes and limit crop growth in soils where nutrients and water are scarce.",
keywords = "Hordeum vulgare, penetration resistance, pore diameter, bulk density, soil chemistry, Hordeum-vulgare-L, root elongation, soil strength, moisture availability, physical conditions, Scotland, dry bulk density, seminal roots, barley, mechanical impedance, soil porosity, wheat triticum-aestivum, growth, macroporosity, water-stress, abiotic stress",
author = "Valentine, {Tracy A.} and Hallett, {Paul D.} and Kirsty Binnie and Young, {Mark W.} and Squire, {Geoffrey R.} and Cathy Hawes and Bengough, {A. Glyn}",
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pages = "259--270",
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TY - JOUR

T1 - Soil strength and macropore volume limit root elongation rates in many UK agricultural soils

AU - Valentine, Tracy A.

AU - Hallett, Paul D.

AU - Binnie, Kirsty

AU - Young, Mark W.

AU - Squire, Geoffrey R.

AU - Hawes, Cathy

AU - Bengough, A. Glyn

PY - 2012/7

Y1 - 2012/7

N2 - Background and Aims Simple indicators of crop and cultivar performance across a range of soil types and management are needed for designing and testing sustainable cropping practices. This paper determined the extent to which soil chemical and physical properties, particularly soil strength and pore-size distribution influences root elongation in a wide range of agricultural top soils, using a seedling-based indicator. Methods Intact soil cores were sampled from the topsoil of 59 agricultural fields in Scotland, representing a wide geographic spread, range of textures and management practices. Water release characteristics, dry bulk density and needle penetrometer resistance were measured on three cores from each field. Soil samples from the same locations were sieved, analysed for chemical characteristics, and packed to dry bulk density of 1·0 g cm−3 to minimize physical constraints. Root elongation rates were determined for barley seedlings planted in both intact field and packed soil cores at a water content close to field capacity (–20 kPa matric potential). Key Results Root elongation in field soil was typically less than half of that in packed soils. Penetrometer resistance was typically between 1 and 3 MPa for field soils, indicating the soils were relatively hard, despite their moderately wet condition (compared with <0·2 MPa for packed soil). Root elongation was strongly linked to differences in physical rather than chemical properties. In field soil root elongation was related most closely to the volume of soil pores between 60 µm and 300 µm equivalent diameter, as estimated from water-release characteristics, accounting for 65·7 % of the variation in the elongation rates. Conclusions Root elongation rate in the majority of field soils was slower than half of the unimpeded (packed) rate. Such major reductions in root elongation rates will decrease rooting volumes and limit crop growth in soils where nutrients and water are scarce.

AB - Background and Aims Simple indicators of crop and cultivar performance across a range of soil types and management are needed for designing and testing sustainable cropping practices. This paper determined the extent to which soil chemical and physical properties, particularly soil strength and pore-size distribution influences root elongation in a wide range of agricultural top soils, using a seedling-based indicator. Methods Intact soil cores were sampled from the topsoil of 59 agricultural fields in Scotland, representing a wide geographic spread, range of textures and management practices. Water release characteristics, dry bulk density and needle penetrometer resistance were measured on three cores from each field. Soil samples from the same locations were sieved, analysed for chemical characteristics, and packed to dry bulk density of 1·0 g cm−3 to minimize physical constraints. Root elongation rates were determined for barley seedlings planted in both intact field and packed soil cores at a water content close to field capacity (–20 kPa matric potential). Key Results Root elongation in field soil was typically less than half of that in packed soils. Penetrometer resistance was typically between 1 and 3 MPa for field soils, indicating the soils were relatively hard, despite their moderately wet condition (compared with <0·2 MPa for packed soil). Root elongation was strongly linked to differences in physical rather than chemical properties. In field soil root elongation was related most closely to the volume of soil pores between 60 µm and 300 µm equivalent diameter, as estimated from water-release characteristics, accounting for 65·7 % of the variation in the elongation rates. Conclusions Root elongation rate in the majority of field soils was slower than half of the unimpeded (packed) rate. Such major reductions in root elongation rates will decrease rooting volumes and limit crop growth in soils where nutrients and water are scarce.

KW - Hordeum vulgare

KW - penetration resistance

KW - pore diameter

KW - bulk density

KW - soil chemistry

KW - Hordeum-vulgare-L

KW - root elongation

KW - soil strength

KW - moisture availability

KW - physical conditions

KW - Scotland

KW - dry bulk density

KW - seminal roots

KW - barley

KW - mechanical impedance

KW - soil porosity

KW - wheat triticum-aestivum

KW - growth

KW - macroporosity

KW - water-stress

KW - abiotic stress

U2 - 10.1093/aob/mcs118

DO - 10.1093/aob/mcs118

M3 - Article

VL - 110

SP - 259

EP - 270

JO - Annals of Botany

JF - Annals of Botany

SN - 0305-7364

IS - 2

ER -