Search results for "0403 Geology"

showing 2 items of 2 documents

Isotope fractionation of zinc in the paddy rice soil-water environment and the role of 2’deoxymugineic acid (DMA) as zincophore under Zn limiting con…

2021

Non-traditional stable isotope systems are increasingly used to study micronutrient cycling and acquisition in terrestrial ecosystems. We previously proposed for zinc (Zn) a conceptual model linking observed isotope signatures and fractionations to biogeochemical processes occurring in the rice soil environment and we suggested that 2’deoxymugineic acid (DMA) could play an important role for rice during the acquisition of Zn when grown under Zn limiting conditions. This proposition was sustained by the extent and direction of isotope fractionation observed during the complexation of Zn with DMA synthesised in our laboratory. Here we report a new set of experimental data from field and labor…

Geochemistry & GeophysicsBiogeochemical cycleGoethite010504 meteorology & atmospheric scienceschemistry.chemical_elementZinc010502 geochemistry & geophysics01 natural sciencesAlkali soilIsotope fractionationPRECISE ZNMUGINEIC ACIDGeochemistry and PetrologySILICON ISOTOPE0402 Geochemistry0105 earth and related environmental sciencesRhizosphereScience & TechnologyStable isotope ratioORYZA-SATIVA L.food and beveragesGeologyIRON ACQUISITIONTOXIC LEVELSchemistryMETAL-IONS0403 GeologyMASS BIAS CORRECTIONEnvironmental chemistryvisual_artSoil waterPhysical Sciencesvisual_art.visual_art_medium0406 Physical Geography and Environmental GeoscienceORGANIC-ACIDSGeologyPLANT-SYSTEM
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Giant barocaloric effects over a wide temperature range in superionic conductor AgI

2017

Current interest in barocaloric effects has been stimulated by the discovery that these pressure-driven thermal changes can be giant near ferroic phase transitions in materials that display magnetic or electrical order. Here we demonstrate giant inverse barocaloric effects in the solid electrolyte AgI, near its superionic phase transition at ~420 K. Over a wide range of temperatures, hydrostatic pressure changes of 2.5 kbar yield large and reversible barocaloric effects, resulting in large values of refrigerant capacity. Moreover, the peak values of isothermal entropy change (60 J K−1 kg−1 or 0.34 J K−1 cm−3) and adiabatic temperature changes (18 K), which we identify for a starting tempera…

Phase transitionMaterials scienceThermal propertiesScienceHydrostatic pressureGeneral Physics and Astronomy02 engineering and technologyElectrolytePropietats tèrmiques7. Clean energy01 natural sciencesGeneral Biochemistry Genetics and Molecular BiologyIsothermal processArticle0103 physical sciencesThermalMagnetic propertiesFast ion conductorlcsh:Science010306 general physicsAdiabatic processMultidisciplinaryCondensed matter physicsPropietats magnètiquesQGeneral ChemistryAtmospheric temperature rangeCiència dels materials021001 nanoscience & nanotechnologyMaterials science0403 Geologylcsh:Q0210 nano-technologyNature Communications
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