Calcite and aragonite were precipitated by diffusing CO2 and NH3 gases into aqueous solutions containing Ca, Sr, Mg and ammonium ions at three different temperatures 12.5, 25 and 37.5 °C. Trace element incorporation and isotopic fractionation of Sr and Ca were measured as function of temperature and precipitation rate.Calcit und Aragonit wurden durch Diffusion von CO2 und NH3 Gasen in wässrigen Lösungen, die Ca, Sr, Mg und Ammoniumionen bei drei verschiedenen Temperaturen 12,5, 25 und 37,5 ° C ausgefällt . Spurenelement Einbau und Isotopenfraktionierung von Sr und Ca wurden als Funktion der Temperatur und Niederschlagsmenge gemessen
In recent years, stalagmites have become an important archive for paleoclimate. Several studies abou...
The oxygen isotope fractionation between HCO3-/CO 32- and H2O was determined experimentally in order...
In order to study Strontium (Sr) partitioning and isotope fractionation of Sr and Calcium (Ca) in ca...
Calcite and aragonite were precipitated by diffusing CO2 and NH3 gases into aqueous solutions contai...
Trace elements incorporation of certain trace elements like strontium (Sr) and magnesium (Mg) among ...
In order to study Strontium (Sr) partitioning and isotope fractionation of Sr and Calcium (Ca) in ar...
In order to study Strontium (Sr) partitioning and isotope fractionation of Sr and Calcium (Ca) in ca...
Ca isotope fractionation during inorganic calcite formation was experimentally studied by spontaneou...
This dissertation is about trace element and isotope fractionation in natural and laboratory-synthes...
Highlights • Sr isotope composition in different minerals is an excellent proxy, that can be u...
In order to study Strontium (Sr) partitioning and isotope fractionation of Sr and Calcium (Ca) in ar...
AbstractIn order to apply Sr/Ca and 44Ca/40Ca fractionation during calcium carbonate (CaCO3) formati...
Mg/Ca and Sr/Ca ratios in calcium carbonate are important components of many palaeoclimate studies. ...
AbstractCarbonate clumped isotopes are applied to an increasing number of geological archives to add...
Calcium is the fifth most abundant element of the silicate Earth. Its interest results from its abun...
In recent years, stalagmites have become an important archive for paleoclimate. Several studies abou...
The oxygen isotope fractionation between HCO3-/CO 32- and H2O was determined experimentally in order...
In order to study Strontium (Sr) partitioning and isotope fractionation of Sr and Calcium (Ca) in ca...
Calcite and aragonite were precipitated by diffusing CO2 and NH3 gases into aqueous solutions contai...
Trace elements incorporation of certain trace elements like strontium (Sr) and magnesium (Mg) among ...
In order to study Strontium (Sr) partitioning and isotope fractionation of Sr and Calcium (Ca) in ar...
In order to study Strontium (Sr) partitioning and isotope fractionation of Sr and Calcium (Ca) in ca...
Ca isotope fractionation during inorganic calcite formation was experimentally studied by spontaneou...
This dissertation is about trace element and isotope fractionation in natural and laboratory-synthes...
Highlights • Sr isotope composition in different minerals is an excellent proxy, that can be u...
In order to study Strontium (Sr) partitioning and isotope fractionation of Sr and Calcium (Ca) in ar...
AbstractIn order to apply Sr/Ca and 44Ca/40Ca fractionation during calcium carbonate (CaCO3) formati...
Mg/Ca and Sr/Ca ratios in calcium carbonate are important components of many palaeoclimate studies. ...
AbstractCarbonate clumped isotopes are applied to an increasing number of geological archives to add...
Calcium is the fifth most abundant element of the silicate Earth. Its interest results from its abun...
In recent years, stalagmites have become an important archive for paleoclimate. Several studies abou...
The oxygen isotope fractionation between HCO3-/CO 32- and H2O was determined experimentally in order...
In order to study Strontium (Sr) partitioning and isotope fractionation of Sr and Calcium (Ca) in ca...