Dataset - B2FIND

Dissolved concentrations of major elements and water isotopes for water sampl...

Water samples were filtered to 0.2 micron prior to measurement. Samples for cation analysis were acidified in the field to pH < 2 using 6N HNO3. Cation concentrations were...

Seawater carbonate chemistry and blood acid-base balance and other blood para...

Global ocean acidification is expected to chronically lower the pH to 7.3 (>2200 µatm seawater pCO2) by the year 2300. Acute hypercapnia already occurs along the South...

Table 1. pH, Temperature, conductivity and hydrochemistry of samples

Carbon dioxide deep geological storage, especially in deep saline aquifers, is one of the preferred technological options to mitigate the effects of greenhouse gases emissions....

Compilation of major and trace element concentrations in mesopelagic and othe...

Organisms accumulate major and trace elements (including metals) directly from the external environment and/or indirectly through diet. As such, their elemental composition can...

Seawater carbonate chemistry and mechanical properties of shark teeth

Ocean acidification can cause dissolution of calcium carbonate minerals in biological structures of many marine organisms, which can be exacerbated by warming. However, it is...

Table S1: chemical measurements and saturation indices of lake water and pore...

This dataset has no description

Wavelength Dispersive Electron Microprobe Analysis of single glass shards (WD...

This dataset has no description

Chemical composition of water samples from freshwater ponds, rice paddies, sh...

Missing values correspond to concentrations below detection. DIC not measured for May 2012 samples, so charge imbalance error (CIB) not calculated. Salinity calculated from...

(Table 3) Chemical composition of water samples from the shallow aquifer in s...

On 2017-05-15 it was noted that the parameter Chlorine had erroneously been named 'Chlorinity' in this table, this was corrected ('Chlorinity' replaced by 'Chlorine', same unit).

(Table 1) Physicochemical composition of Milos, Dominica and Iceland surface ...

The Na - K geothermometer is in the form from Fournier (1979): T (°C) = (1217/log(Na/K) + 1.483) - 273.15; The Na - K - Ca geothermometer equation is in the form from Henley et...