Add to ORKGThe coefficient fH used in the seawater alkalinity method of Anderson and Robinson (1946), has been redetermined at 25°C. We have found that fH = 0.741 ±0,005 for salinities between 30‰ and 41‰…
To the best of our knowledge, one or more authors of this paper were federal employees when contribu...
Spectrophotometric procedures utilizing sulfonephthalein indicators provide rapid, quantitative meas...
The apparent dissociation constants, pK\u27, of five sulfonephthalein indicators (thymol blue, bromo...
Alkalinity values in the top few hundred meters in Baffin Bay were about 100 μeq kg—1 above those ex...
The solid material obtained upon freeze-drying sea water is not a true measure of salinity since it ...
We have calculated the effect of the increased alkalinity, total carbon dioxide and silica content o...
The emission of anthropogenic carbon is leading to the influx of additional CO2 to the atmosphere an...
Accurately measuring the marine CO2 system is imperative to assess the effect of oceanic uptake of a...
The ranges of alkalinity and pH in the southern Chesapeake Bay and the James River estuary were 2.25...
The titration system is described that was used to measure the total alkalinity of seawater (TA) dur...
Two definitions of salinity have been in use since the early part of the present century (Knudsen 19...
Modified spectrophotometric procedures are presented for the determination of seawater total alkalin...
A method for determining the amount of potassium in ocean water has been described. With this proced...
Evidence of ocean acidification (OA) throughout the global ocean has galvanized some coastal communi...
Boric acid-borate apparent dissociation constants were determined in synthetic media and in seawater...
To the best of our knowledge, one or more authors of this paper were federal employees when contribu...
Spectrophotometric procedures utilizing sulfonephthalein indicators provide rapid, quantitative meas...
The apparent dissociation constants, pK\u27, of five sulfonephthalein indicators (thymol blue, bromo...
Alkalinity values in the top few hundred meters in Baffin Bay were about 100 μeq kg—1 above those ex...
The solid material obtained upon freeze-drying sea water is not a true measure of salinity since it ...
We have calculated the effect of the increased alkalinity, total carbon dioxide and silica content o...
The emission of anthropogenic carbon is leading to the influx of additional CO2 to the atmosphere an...
Accurately measuring the marine CO2 system is imperative to assess the effect of oceanic uptake of a...
The ranges of alkalinity and pH in the southern Chesapeake Bay and the James River estuary were 2.25...
The titration system is described that was used to measure the total alkalinity of seawater (TA) dur...
Two definitions of salinity have been in use since the early part of the present century (Knudsen 19...
Modified spectrophotometric procedures are presented for the determination of seawater total alkalin...
A method for determining the amount of potassium in ocean water has been described. With this proced...
Evidence of ocean acidification (OA) throughout the global ocean has galvanized some coastal communi...
Boric acid-borate apparent dissociation constants were determined in synthetic media and in seawater...
To the best of our knowledge, one or more authors of this paper were federal employees when contribu...
Spectrophotometric procedures utilizing sulfonephthalein indicators provide rapid, quantitative meas...
The apparent dissociation constants, pK\u27, of five sulfonephthalein indicators (thymol blue, bromo...