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  • Wiley  (3)
  • Geography  (3)
  • 1
    Online Resource
    Online Resource
    Wiley ; 2021
    In:  Journal of Plant Nutrition and Soil Science Vol. 184, No. 6 ( 2021-12), p. 688-695
    In: Journal of Plant Nutrition and Soil Science, Wiley, Vol. 184, No. 6 ( 2021-12), p. 688-695
    Abstract: Manganese (Mn) is an essential nutrient for plant growth and a key factor driving litter decomposition. Nitrogen (N) deposition is expected to enhance soil Mn availability via soil acidification, and subsequently to increase plant Mn concentrations. Aims We aimed to quantify the responses of Mn concentrations in green and senesced shoots at both species and community levels to N addition, and determine whether N addition would decrease Mn retranslocation efficiency during plant senescence. Methods We examined the changes of Mn concentrations in soil and in green and senesced shoots of all plant species across multiple N addition rates ranging from 0 to 50 g N m −2 y −1 in a temperate steppe after six years treatments. Plant Mn retranslocation efficiency were quantified at species, life form, and community levels. The relationship between plant Mn nutritional parameters and soil Mn availability across the N addition gradient was analyzed. Results There were positive correlations between plant Mn concentrations and N addition rates for most species. Relative to the control plots, community‐level mean Mn concentration in green and senesced shoots in the plots received the highest level of N addition increased by 137.50% (from 0.19 mg kg −1 to 0.08 mg kg −1 ) and 187.50% (from 0.23 mg kg −1 to 0.08 mg kg −1 ), respectively. There was no correlation between Mn retranslocation efficiency and N addition rates at species, life form and community levels. Plant Mn status was weakly correlated with soil Mn concentrations for most species. Conclusions Plant Mn retranslocation showed conserved responses to increasing N addition rates, which would be an adaptive strategy for plants in face of N‐induced higher soil Mn availability.
    Type of Medium: Online Resource
    ISSN: 1436-8730 , 1522-2624
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2021
    detail.hit.zdb_id: 1481142-X
    detail.hit.zdb_id: 1470765-2
    detail.hit.zdb_id: 200063-5
    SSG: 12
    SSG: 13
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  • 2
    Online Resource
    Online Resource
    Wiley ; 1995
    In:  Journal of Metamorphic Geology Vol. 13, No. 6 ( 1995-11), p. 659-675
    In: Journal of Metamorphic Geology, Wiley, Vol. 13, No. 6 ( 1995-11), p. 659-675
    Abstract: Abstract In the Su‐Lu ultrahigh‐ P terrane, eastern China, many coesite‐bearing eclogite pods and layers within biotite gneiss occur together with interlayered metasediments now represented by garnet‐quartz‐jadeite rock and kyanite quartzite. In addition to garnet + omphacite + rutile + coesite, other peak‐stage minerals in some eclogites include kyanite, phengite, epidote, zoisite, talc, nyböite and high‐Al titanite. The garnet‐quartz‐jadeite rock and kyanite quartzite contain jadeite + quartz + garnet + rutile ± zoisite ± apatite and quartz + kyanite + garnet + epidote + phengite + rutile ± omphacite assemblages, respectively. Coesite and quartz pseudomorphs after coesite occur as inclusions in garnet, omphacite, jadeite, kyanite and epidote from both eclogites and metasediments. Study of major elements indicates that the protolith of the garnet‐quartz jadeite rock and the kyanite quartzite was supracrustal sediments. Most eclogites have basaltic composition; some have experienced variable ‘crustal’contamination or metasomatism, and others may have had a basaltic tuff or pyroclastic rock protolith. The Su‐Lu ultrahigh‐ P rocks have been subjected to multi‐stage recrystallization and exhibit a clockwise P‐T path. Inclusion assemblages within garnet record a pre‐eclogite epidote amphibolite facies metamorphic event. Ultrahigh‐ P peak metamorphism took place at 700–890° C and P 〉 28 kbar at c . 210–230 Ma. The symplectitic assemblage plagioclase + hornblende ± epidote ± biotite + titanite implies amphibolite facies retrogressive metamorphism during exhumation at c . 180–200 Ma. Metasedimentary and metamafic lithologies have similar P‐T paths. Several lines of evidence indicate that the supracrustal rocks were subducted to mantle depths and experienced in‐situ ultrahigh‐ P metamorphism during the Triassic collision between the Sino‐Korean and Yangtze cratons.
    Type of Medium: Online Resource
    ISSN: 0263-4929 , 1525-1314
    URL: Issue
    RVK:
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1995
    detail.hit.zdb_id: 2020499-1
    SSG: 13
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  • 3
    Online Resource
    Online Resource
    Wiley ; 2009
    In:  Soil Science Society of America Journal Vol. 73, No. 6 ( 2009-11), p. 1995-2001
    In: Soil Science Society of America Journal, Wiley, Vol. 73, No. 6 ( 2009-11), p. 1995-2001
    Abstract: Glyphosate [ N ‐(phosphonomethyl)glycine] is a nonselective, postemergence herbicide that contains multiple functional groups, which can form strong coordination with metal cations to give bidentate and tridentate complex es. The complexation of glyphosate with metal cations may affect their distribution and bioavailability in soils. Adsorption kinetics of glyphosate and Cu(II) alone and together were studied using a continuous flow experimental setup on two soils with different characteristics at pH5.5. Four kinetic models, i.e., the Lagergren first‐order, pseudo‐second‐order, Elovich, and power function equations, were successfully used to describe their adsorption kinetics. Among the four models, the Lagergren first‐order kinetic model fit the experimental data of glyphosate and Cu(II) adsorption the best. Glyphosate significantly increased the adsorption quantity of Cu(II) on the Red soil (a Hapludult or Udic Ferrosol), due to the fact that Cu(II) was adsorbed on the sites where glyphosate had been strongly adsorbed. Glyphosate decreased the adsorption of Cu(II) on the Wushan soil (a Haplaquept or Anthrosol), however, because adsorption of glyphosate on this soil was weak and the complex of glyphosate and Cu(II) tended to be highly soluble in water, thus preventing Cu(II) from exchanging with Ca 2+ and Mg 2+ ions on the soil surface. On the other hand, the presence of Cu(II) decreased the adsorption of glyphosate on both soils, which may be attributed to the lower affinity of the Cu(II)–glyphosate complex to the soils than glyphosate alone.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2009
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    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
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