Lake Pontchartrain Basin:  Bottom Sediments and Related Environmental Resources

Continuous Sediment Sampling and Analysis System

Appendix A.  Quality Assurance and Control

Several steps were taken to ensure that the systems used to perform the survey were operating properly at all times. The methods for the quality assurance and control were documented in the Quality Assurance Project Plan (QAPP) for this project (CAIS, 1997). The topics addressed during the quality control measures are addressed in the following text.

    • Precision and accuracy
    • Total sample concentrations
    • Interlab sample comparison

Precision and Accuracy

A replicate sample analysis was performed for the NIST 2704 wafer. Table A1 shows the results of the replicate analyses processed from the NIST Standard 2704. The precision and accuracy results were generated by repeating XRF analysis on the same wafer at least five times. All analytes for the filter sample were within the expected range of precision and accuracy.

Table A1.  XRF Data Quality Measurements for Filters

System Analyte Precisiona Precisionb Precisionc Accuracyc
Al 2.4% 2.3% 25% 25%
Si 1.4% 5.6% 25% 25%
  S 5.4% 8.5% 25% 25%
  Fe 1.2% 1.8% 25% 25%
  Ca 1.6% 3.6% 25% 25%
  K 0.7% N/A 25% N/A
  Ti 1.0% 3.7% 25% 25%
  Mg 4.9% 2.8% 25% 25%
ppm Cr 4.7% 3.9% 25% 25%
  Mn 2.6% 1.7% 25% 25%
  Ni 19.3% 10.2% 25% 25%
  Cu 1.8% 0.4% 25% 25%
  Zn 1.5% 0.2% 25% 25%
  Zr 9.0% 3.9% 25% 25%
  Sr 6.8% 3.9% 25% 25%
  Cd 28.4% 12.2% 40% 40%
  Sb 37.9% 9.0% 40% 40%
  Sn 14.6% 13.9% 40% 40%
  Ba 8.3% 3.7% 25% 25%
  Pb 2.3% 1.7% 25% 25%

a Relative standard deviation based on replicate analysis of NIST 2704 filter.
b Difference from true value based on replicate analysis of NIST 2704 filter.
c Acceptance/rejection values.

Total Sample Concentration

Analytical totals for the samples analyzed from the 1997 Lake Pontchartrain survey ranged from approximately 85% to 115%. This range in totals was reflected in the individual elemental concentrations and caused a scatter effect in the final results. When the data were plotted in a metal to metal format that generally shows correspondence, there was only scatter showing little to no correlation. The problem of variable total concentration has been solved by normalizing the data to a 90% total. By normalizing the data to 90%, the variation is greatly reduced and the data plots show considerably less scatter. Figure A1 gives an example of the relationship of aluminum to silicon for the 1997 Lake Pontchartrain data. With the exception of a few samples, the correlation gives a reasonable regression. In addition, mean aluminum values for normalized 1997 data (6.51 wt%) and for normalized 1996 data (6.89 wt%) are very close. The 1997 aluminum range was 3.1 to 9.89 wt% as compared to 2.0 to 9.19 wt% for the 1996 data.

While 90% is somewhat arbitrary, it was chosen because the structural H2O was determined to be relatively consistent at 8% to 9%, and elemental Na values were consistently between 0.5% and 2%. The consideration of the structural H2O and Na, along with the remaining analytes should account for >99% of the elemental makeup of the sample.

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Figure A1.  Normalized aluminum to silicon plot for the 1997 Lake Pontchartrain data.


Interlab Sample Comparison

In order to test the quality of the data, six samples from the 1997 Lake Pontchartrain survey were sent to two labs, the XRF lab at Georgia State University (GSU) and the analytical lab at Skidaway Institute of Oceanography (Skidaway). The samples were chosen not because of quality or location but because of extra sediment collected at these particular stations. The samples were collected during the 1997 survey as bulk sediment slurry samples from the CS processor at approximately the same time that the corresponding CS filter sample was collected. These samples were dried and archived for future use. Figure A2 shows the results of the interlab comparison of the six Lake Pontchartrain samples. Five of the samples show a good correlation. One sample, CAIS Sample 244, appeared to be out of line with its counterparts analyzed by GSU and Skidaway. Upon reanalyses, the aluminum concentration remained the same as previously reported. Since this sample was originally analyzed in 1997, and now in 1998 with the same results, it is mostly likely not a random error on the part of the XRF. Analytical methods, such as XRF and atomic absorption, may not always agree usually reflecting the differences in sample preparation. However, it was shown by figure A2 that the data reflect the same relative difference from one method to another.

The GSU samples were processed into fused glass disks and analyzed by a Rigaku 3070 wavelength-dispersive spectrometer utilizing a side-window Rh target X-ray tube (XRF). The sediment was fused using lithium borate flux by heating in a furnace at 1100C. The ratio of flux to sediment was 9:1, producing a glass disk that was essentially a borate glass with sediment dissolved in it.

The Skidaway samples were processed using a lithium metaborate fusion and analyzed by an atomic absorption spectrophotometer (AA) following EPA Method 7020. Approximately 250 mg of sample was placed in a clean alumina crucible and heated at 900C for 30 min. After cooling, the sample was reweighed and percent loss on ignition was calculated. The ratio of lithium metaborate flux to sample powder is 4:1. A total of 100 mg of ashed sample with 400 mg flux was thoroughly mixed and then placed in a graphite crucible. The crucible was then placed into a muffle furnace at 1050C for 8 min., removed, swirled, and returned to the oven for another 7 min. The glass beads from the crucibles were poured directly into a wide-mouth bottle containing 50 mL of 1.5N HNO3 spiked with 10 ppm Ge. The sample was vigorously shaken until all the glass was dissolved. The sample was then analyzed by the AA for aluminum content.

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Figure A2.  Interlab sample comparison.


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