This method was designed for the analysis of phosphatic shells. All measurements are best done by weight, or at the very least using weight-calibrated pipettes. It is wise to prepare a set of blanks in parallel with the unknowns. Blank subtraction will be necessary in case of contamination from the acid or elsewhere.

Sample preparation

  1. Thorougly rinse the samples in deionized water and dry at 110°C for one hour.
  2. Mix up 100 ml of 1:5 HCl (~2.4 molar).
  3. Weigh 5 to 50 mg of shell sample into a 13 ml test tube.
  4. Add 1 ml of the 1:5 HCl and let sit overnight to dissolve.
  5. Add 9 ml of water to bring the total volume to 10 ml. Again, it is recommended that measurements be done by weight.
  6. To rinsed ion chromatograph autosampler vials add 4.5 ml of water, and then 0.5 ml of the sample solution, to yield an additional dilution factor of ~10. In this solution, 5 to 50 mg of shell is effectively diluted by factors of 20,000 to 2000, respectively (10 ml/0.005 g * 10 to 10 ml/0.05 g * 10, respectively).
  7. You may wish to rinse, dry, and weigh the organic residue left after shell dissolution. This will allow you to calculate more accurately the composition of the phosphate component.

Prepare the anion standard

Ion Stock concentration, ppm ml used Standard/1, ppm
F- 1000 1 10
Acetate 1000 0.1 1
Formate 1000 0.1 1
SO42- 1000 1 10
Oxylate 1000 0.5 5
PO43- 3080** 4 123.2
* 1000 ppm as N, 4428 ppm as NO3-.
** 1000 ppm as P, 3080 ppm as PO43-.

 

Pour Standard/1 into a clean 125 ml plastic bottle. Transfer appropriate numbers of 5.5 ml aliquots of DI water and Standard/1 to four other bottles. The numbers of 5.5 ml aliquots are as follows:

 

  Standard/1 Standard/2 Standard/5 Standard/10 Standard/20
5.5 ml Aliquots of DI water - 5 8 9 9
5.5 ml Aliquots of Standard/1 - 5 2 1 1 from Standard/2
Ion Resulting concentrations, ppm
F- 10 5 2 1 0.5
Acetate 1 0.5 0.2 0.1 0.05
Formate 1 0.5 0.2 0.1 0.05
SO42- 10 5 2 1 0.5
Oxylate 5 2.5 1 0.5 0.25
PO43- 123.2 61.6 24.6 12.3 6.16

 

The result will be 56 ml of Standard/1, 49.5 ml of Standard/2, and 55 ml of the others.

Prepare the cation standard

In general, standards should be similar in composition to the samples being analyzed. Since samples vary enormously, you may want to start with a generally useful standard. For this, dilute the following stock solutions in a 100 ml volumetric flask.

 

Ion Stock concentration, ppm ml used Standard/1, ppm
Li+ 1000 0.05 0.5
Na+ 1000 0.5 5
NH4+ 1000 0.1 1
K+ 1000 0.1 1
Mg2+ 1000 0.3 3
Ca2+ 1000 10 100
Sr2+ 1000 0.2 2

 

Pour Standard/1 in to a clean 125 ml plastic bottle. Transfer appropriate numbers of 5.5 ml aliquots of DI water and Standard/1 to four other bottles. The numbers of 5.5 ml aliquots are as follows:

 

  Standard/1 Standard/2 Standard/5 Standard/10 Standard/20
5.5 ml Aliquots of DI water - 5 8 9 9
5.5 ml Aliquots of Standard/1 - 5 2 1 1 from Standard/2
Ion Resulting concentrations, ppm
Li+ 0.5 0.25 0.1 0.05 0.025
Na+ 5 2.5 1 0.5 0.25
NH4+ 1 0.5 0.2 0.1 0.05
K+ 1 0.5 0.2 0.1 0.05
Mg2+ 3 1.5 0.6 0.3 0.15
Ca2+ 100 50 20 10 5
Sr2+ 2 1 0.4 0.2 0.1

 

The result will be 56 ml of Standard/1, 49.5 ml of Standard/2, and 55 ml of the others.

Analysis setup

Run DI water washes before the unknowns and the blanks. Monitor analytical quality with one or more standards run as unknowns within or at the end of the run. Set all dilution factors to 1. Off line subtract the blanks and then apply the dilution factors.

Note on the shell dissolution reaction

The shell dissolution reaction is:

 

Ca5(PO4)3F + 10HCl = 5CaCl2 + 3H3PO4 + HF.

 

Therefore, on a molar basis 10 times as much HCl is needed as there is shell phosphate. The 1 ml of HCl used to dissolve the sample is ~2.4 M, and contains 2.4*10-3 moles HCl. 5 to 50 mg of fluorapatite shell material has 1*10-5 to 10*10-5 moles of Ca5(PO4)3F. So, remembering that 10 times as much HCl is needed as there is fluorapatite, there is an excess of HCl ranging from 24 (5 mg shell) to 2.4 (50 mg shell). The shell material, however, is not pure apatite and contains considerable organic material, so the actual excess of HCl is larger. This organic material will remain after dissolution and may resemble a transparent version of the original shell.

Note on acid purity

It is important that the acids be reasonably pure. The table below shows several runs made with 1:1000 HCl and HNO3, both undistilled reagent grade and distilled (in-house two-bottle Teflon still), and reagent grade acetic acid. As can be seen, all of the acids are very clean, with most components near or below detection limits. HCl is recommended since the chloride peak will only interfere with Cl- and NO2-, which are unimportant in these samples. HNO3, on the other hand, will potentially interfere with phosphate, which is important.

 

  HCl ACS 1 HCl ACS 2 HCl distilled HNO3 ACS HNO3 distilled HAc ACS Blank Blank
F   0.002 0.002 0.002 0.001 0.001 0.001  
Glycolate   0.04 0.00 0.01 0.01   0.00 0.01
Acetate       0.01   590.14    
Formate     0.01          
Propionate     0.05   0.02     0.02
Methyl-sulfonate 0.01 0.01            
Cl 406 410 366   0.00     0.01
NO2   0.00 0.00   0.08 0.00   0.00
SO4                
Oxalate 0.00     -280 -268     0.02
Br         0.01      
NO3 0.00 0.06     98 0.09 0.03 0.01
PO4 0.01 0.02 0.04 0.01 0.01 0.01 0.01 0.02
Li                
Na 0.01 0.00 0.02   0.00 0.00 0.01 0.02
NH4                
K                
Mg 0.00           0.01 0.02
Ca 0.01 0.00 0.00 0.00 0.00   0.05 0.06
ACS = American Chemical Society, reagent grade acid, not distilled.
Blank cells indicate that no peak was detected.
Black cells indicate that added acid peaks either added the anion of interest, or caused a large interference on another ion.