971 resultados para mepiquat chloride

(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structurally bound (SBC) fractions of chloride component in serpentinized ultramafic rocks from DSDP Site 558

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(Fig. 1 & 2) Sea water and Paralomis granulosa haemolymph magnesium, calcium and sulphate, sodium and chloride fractions

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(Table T1) Chloride and sulphate content, and sulphur isotope ratios of sulphate in interstitial waters from ODP Leg 181 sites

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(Table 1) Organic carbon and calcium carbonate contents of sediment minicores and interstitial-water salinity, chloride concentrations, and charg-imbalance of ODP Leg 119 Prydz Bay sites

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(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structurally bound (SBC) fractions of chloride component in serpentinized ultramafic rocks from ODP Site 153-920D

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(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structurally bound (SBC) fractions of chloride component in serpentinized ultramafic rocks from ODP Site 107-651A

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(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structurally bound (SBC) fractions of chloride component in serpentinized ultramafic rocks from ODP Site 109-670A

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(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structurally bound (SBC) fractions of chloride component in serpentinized ultramafic rocks from ODP Site 147-895E

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(Table 7a) Azide, sulfide, ammonium chloride and thiosulfate influences on carbon-14 dioxide assimilation rates in water samples from the Broken Spur and TAG hydrothermal fields

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(Table 1) Chloride and bromide concentrations and Br-/Cl- molar ratios in pore fluids of ODP Hole 134-833B

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(Table 2) Contents of chloride components in serpentinized ultramafic rocks from ODP Site 107-651A

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(Figure 5) Vertical distribution of chloride and sulfate ion concentrations in soil waters from soil profiles in the Badain Jaran Desert, Northern China

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(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structurally bound (SBC) fractions of chloride component in serpentinized ultramafic rocks from DSDP Site 566

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(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structurally bound (SBC) fractions of chloride component in serpentinized ultramafic rocks from DSDP Site 570

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(Figure 5) Pore-water concentration of chloride in sediment core GeoB11913 from the Vodyanitskii mud volcano

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