Growth, morphological and physiological responses of alfalfa (Medicago sativa) to phosphorus supply in two alkaline soils

Background and aims Phosphorus (P) deficiency is a major problem for alfalfa (Medicago sativa) productivity on alkaline soils on the Loess Plateau, China. Our aim was to investigate growth, morphological and physiological responses of alfalfa to P supply in two alkaline soils when water supply is li...

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Published inPlant and soil Vol. 416; no. 1/2; pp. 565 - 584
Main Authors He, Honghua, Peng, Qi, Wang, Xia, Fan, Chenbin, Pang, Jiayin, Lambers, Hans, Zhang, Xingchang
Format Journal Article
LanguageEnglish
Published Cham Springer 01.07.2017
Springer International Publishing
Springer Nature B.V
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Abstract Background and aims Phosphorus (P) deficiency is a major problem for alfalfa (Medicago sativa) productivity on alkaline soils on the Loess Plateau, China. Our aim was to investigate growth, morphological and physiological responses of alfalfa to P supply in two alkaline soils when water supply is limited. Methods A pot experiment was carried out to grow alfalfa in two alkaline soils supplied with different rates of P. Parameters of plant growth and root morphology, rhizosphere pH and carboxylates, and plant concentrations of mineral nutrients were measured. Results Plant growth and nutrient uptake were enhanced by supplying P, but shoot growth was not further increased when P supply was >20 μg P g−1 soil. Specific root length was only responsive to changes in soil P when P supply was low in the loessial soil. The rhizosphere carboxylate amount was significantly greater when no P was supplied than when P was supplied to the loessial soil. The rhizosphere pH was lower than the bulk soil pH, but did not vary with soil P. Conclusions A P supply of 20 μg P g−1 soil was optimal for alfalfa growth. The responses of specific root length and rhizosphere carboxylates depended on soil type.
AbstractList Background and aims Phosphorus (P) deficiency is a major problem for alfalfa (Medicago sativa) productivity on alkaline soils on the Loess Plateau, China. Our aim was to investigate growth, morphological and physiological responses of alfalfa to P supply in two alkaline soils when water supply is limited. Methods A pot experiment was carried out to grow alfalfa in two alkaline soils supplied with different rates of P. Parameters of plant growth and root morphology, rhizosphere pH and carboxylates, and plant concentrations of mineral nutrients were measured. Results Plant growth and nutrient uptake were enhanced by supplying P, but shoot growth was not further increased when P supply was >20 μg P g−1 soil. Specific root length was only responsive to changes in soil P when P supply was low in the loessial soil. The rhizosphere carboxylate amount was significantly greater when no P was supplied than when P was supplied to the loessial soil. The rhizosphere pH was lower than the bulk soil pH, but did not vary with soil P. Conclusions A P supply of 20 μg P g−1 soil was optimal for alfalfa growth. The responses of specific root length and rhizosphere carboxylates depended on soil type.
Background and aims Phosphorus (P) deficiency is a major problem for alfalfa ( Medicago sativa ) productivity on alkaline soils on the Loess Plateau, China. Our aim was to investigate growth, morphological and physiological responses of alfalfa to P supply in two alkaline soils when water supply is limited. Methods A pot experiment was carried out to grow alfalfa in two alkaline soils supplied with different rates of P. Parameters of plant growth and root morphology, rhizosphere pH and carboxylates, and plant concentrations of mineral nutrients were measured. Results Plant growth and nutrient uptake were enhanced by supplying P, but shoot growth was not further increased when P supply was >20 μg P g −1 soil. Specific root length was only responsive to changes in soil P when P supply was low in the loessial soil. The rhizosphere carboxylate amount was significantly greater when no P was supplied than when P was supplied to the loessial soil. The rhizosphere pH was lower than the bulk soil pH, but did not vary with soil P. Conclusions A P supply of 20 μg P g −1 soil was optimal for alfalfa growth. The responses of specific root length and rhizosphere carboxylates depended on soil type.
Background and aims Phosphorus (P) deficiency is a major problem for alfalfa (Medicago sativa) productivity on alkaline soils on the Loess Plateau, China. Our aim was to investigate growth, morphological and physiological responses of alfalfa to P supply in two alkaline soils when water supply is limited. Methods A pot experiment was carried out to grow alfalfa in two alkaline soils supplied with different rates of P. Parameters of plant growth and root morphology, rhizosphere pH and carboxylates, and plant concentrations of mineral nutrients were measured. Results Plant growth and nutrient uptake were enhanced by supplying P, but shoot growth was not further increased when P supply was >20 [mu]g P g-1 soil. Specific root length was only responsive to changes in soil P when P supply was low in the loessial soil. The rhizosphere carboxylate amount was significantly greater when no P was supplied than when P was supplied to the loessial soil. The rhizosphere pH was lower than the bulk soil pH, but did not vary with soil P. Conclusions A P supply of 20 [mu]g P g-1 soil was optimal for alfalfa growth. The responses of specific root length and rhizosphere carboxylates depended on soil type.
Background and aims Phosphorus (P) deficiency is a major problem for alfalfa (Medicago sativa) productivity on alkaline soils on the Loess Plateau, China. Our aim was to investigate growth, morphological and physiological responses of alfalfa to P supply in two alkaline soils when water supply is limited. Methods A pot experiment was carried out to grow alfalfa in two alkaline soils supplied with different rates of P. Parameters of plant growth and root morphology, rhizosphere pH and carboxylates, and plant concentrations of mineral nutrients were measured. Results Plant growth and nutrient uptake were enhanced by supplying P, but shoot growth was not further increased when P supply was >20 [mu]g P g.sup.-1 soil. Specific root length was only responsive to changes in soil P when P supply was low in the loessial soil. The rhizosphere carboxylate amount was significantly greater when no P was supplied than when P was supplied to the loessial soil. The rhizosphere pH was lower than the bulk soil pH, but did not vary with soil P. Conclusions A P supply of 20 [mu]g P g.sup.-1 soil was optimal for alfalfa growth. The responses of specific root length and rhizosphere carboxylates depended on soil type.
BACKGROUND AND AIMS: Phosphorus (P) deficiency is a major problem for alfalfa (Medicago sativa) productivity on alkaline soils on the Loess Plateau, China. Our aim was to investigate growth, morphological and physiological responses of alfalfa to P supply in two alkaline soils when water supply is limited. METHODS: A pot experiment was carried out to grow alfalfa in two alkaline soils supplied with different rates of P. Parameters of plant growth and root morphology, rhizosphere pH and carboxylates, and plant concentrations of mineral nutrients were measured. RESULTS: Plant growth and nutrient uptake were enhanced by supplying P, but shoot growth was not further increased when P supply was >20 μg P g⁻¹ soil. Specific root length was only responsive to changes in soil P when P supply was low in the loessial soil. The rhizosphere carboxylate amount was significantly greater when no P was supplied than when P was supplied to the loessial soil. The rhizosphere pH was lower than the bulk soil pH, but did not vary with soil P. CONCLUSIONS: A P supply of 20 μg P g⁻¹ soil was optimal for alfalfa growth. The responses of specific root length and rhizosphere carboxylates depended on soil type.
Audience Academic
Author Lambers, Hans
Peng, Qi
Pang, Jiayin
Zhang, Xingchang
Wang, Xia
Fan, Chenbin
He, Honghua
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  givenname: Hans
  surname: Lambers
  fullname: Lambers, Hans
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  givenname: Xingchang
  surname: Zhang
  fullname: Zhang, Xingchang
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Issue 1/2
Keywords )
Phosphorus uptake
Alfalfa
Rhizosphere carboxylates
Root morphology
Mineral nutrients
Language English
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PQPubID 54098
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crossref_citationtrail_10_1007_s11104_017_3242_9
crossref_primary_10_1007_s11104_017_3242_9
springer_journals_10_1007_s11104_017_3242_9
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ProviderPackageCode CITATION
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PublicationCentury 2000
PublicationDate 2017-07-01
PublicationDateYYYYMMDD 2017-07-01
PublicationDate_xml – month: 07
  year: 2017
  text: 2017-07-01
  day: 01
PublicationDecade 2010
PublicationPlace Cham
PublicationPlace_xml – name: Cham
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PublicationSubtitle An International Journal on Plant-Soil Relationships
PublicationTitle Plant and soil
PublicationTitleAbbrev Plant Soil
PublicationYear 2017
Publisher Springer
Springer International Publishing
Springer Nature B.V
Publisher_xml – name: Springer
– name: Springer International Publishing
– name: Springer Nature B.V
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Snippet Background and aims Phosphorus (P) deficiency is a major problem for alfalfa (Medicago sativa) productivity on alkaline soils on the Loess Plateau, China. Our...
Background and aims Phosphorus (P) deficiency is a major problem for alfalfa ( Medicago sativa ) productivity on alkaline soils on the Loess Plateau, China....
BACKGROUND AND AIMS: Phosphorus (P) deficiency is a major problem for alfalfa (Medicago sativa) productivity on alkaline soils on the Loess Plateau, China. Our...
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SubjectTerms Alfalfa
Alkaline soils
Biomedical and Life Sciences
Carboxylates
Chemical properties
China
Ecology
Life Sciences
Loess
Medicago sativa
Morphology
Nutrient concentrations
Nutrient uptake
Nutrients
pH effects
Phosphate fertilizers
Phosphorus
Physiological aspects
physiological response
Physiological responses
Physiology
Plant development
Plant growth
Plant Physiology
Plant Sciences
Plant-soil relationships
Regular Article
Rhizosphere
Soil chemistry
Soil investigations
Soil pH
Soil Science & Conservation
Soil types
Soil water
Soils
Water supply
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Title Growth, morphological and physiological responses of alfalfa (Medicago sativa) to phosphorus supply in two alkaline soils
URI https://www.jstor.org/stable/26651491
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