Important changes in U.S. Geological Survey laboratory analytical methods, reporting conventions, and laboratory sample contamination from 1970-95
[NWQL, National Water Quality Laboratory; BSP, Blind Sample Program; SRWS, Standard Reference Water Sample; NASQAN, National Stream Quality Accounting Network. U.S. Geological Survey memoranda are identified by the originating office and a unique number QWyy_nn (Office of Water Quality) or NLyy_nn (National Water Quality Laboratory), where yy gives the year of the document and nn is a sequential number of the year's memoranda]
[This file is Table 8 in the accompanying Open-File Report]
_____________________________________________________________________________ Constituent Date Description of change (memoranda or references) _____________________________________________________________________________ Common ions 10-01-82 - Sulfate showed a positive bias of about 2 07-31-89 mg/L for concentrations less than 75 mg/L because of interferences in the turbidimetric method that were not blank corrected (QW90_04). 01-01-80 - Residue on Evaporation (ROE) -- Small, 12-31-89 statistically significant trends detected in laboratory measurement bias based on BSP reference sample data (Alexander and others, 1993). Trend is positive for the NWQL and negative for the Atlanta laboratory. 04-01-90 - Sulfate showed a positive bias on the order 03-31-92 of 0.5-3 mg/L for samples with concentrations of 15-75 mg/L. BSP data demonstrate the bias. 04-01-90 - Chloride--Ion chromatography method showed 10-20-92 lack of precision and positive bias on the order of one standard deviation for BSP samples. The ion chromatography method was switched to a colorimetric method in December 1992 (NL93_03). 04-01-90 - Fluoride--Ion chromatography method showed 01-02-94 lack of precision on the order of four standard deviations for BSP samples. The ion chromatography method was switched to an ion- selective electrode method in January 1994 (NL94_03). Nutrients, 10-01-72 - Values changed in the data base to maintain major ions, 09-30-78 consistency in reporting of non-detected and trace ("less-than") values (QW81_18; QW81_22). elements Zeros were replaced with the method reporting limit and a remark code of "<". Un-remarked values equal to the method reporting limit were assigned a remark code of "<". Nutrients Before 1972 The methods of preservation used by field personnel are unknown, but may have included chilling of samples, sulfuric acid, or mercuric chloride. Mercuric chloride was officially recommended for use by the USGS for nitrogen analyses as early as November 1970. 01-05-72 All field offices advised to discontinue use of mercuric chloride as a preservative for nitrogen, phosphorus, and organic carbon because of concerns about instrument interferences and problems of mercuric chloride contamination and safe disposal of wastes (QW72_09). Chilling of samples to 1-40 C. and rapid transport of samples are recommended alternatives. 10-01-80 Mercuric chloride preservatives in tablet form adopted after review of the literature suggests benefits of the use of this biocide (QW80_26). 10-01-86 - Mercuric chloride preservative in liquid 09-30-94 ampoule form adopted (E.L. Skinner, U.S. Geological Survey, written comm., 1990) because of detected ammonia contamination in tablet preservative (QW85_07). 03-27-92 The NWQL began replacing 250 mL brown nutrient bottles and 1 milliliter mercuric chloride ampoules with 125 milliliter brown nutrient bottles and 0.5 milliliter mercuric chloride ampoules for the purpose of reducing the amount of mercuric chloride that is being used in the field and that must be disposed of by the laboratory (QW92_08). 10-01-94 Discontinued the use of mercuric chloride preservative (QW94_16). A USGS study finds no significant differences in analytical results based on samples treated separately with mercuric chloride and chilling. 10-01-94 Discontinued analyses of whole-water ("total") samples for nitrite, nitrate + nitrite, ammonia, and orthophosphorus (QW93_04). From 1973-1994, analyses of these constituents were performed on samples "decanted" in the laboratory. Statistical review of all 1989 data processed in the NWQL suggests that "dissolved" and "total" determinations for these four constituents are not statistically separable. Kjeldahl 10-01-78 - Kjeldahl nitrogen analyzed by method (ammonia 09-30-91 I2552/I4552 without blank correction. plus Positive bias could average more than 0.1 organic) mg/L. nitrogen 01-01-79 - Evidence of occasional periods of positive 12-31-85 bias based on SRWS reference sample measurements at the Denver Central Laboratory (Alexander and others, 1993). 10-01-80 - Positive bias as high as 0.5 mg/L found in 09-30-86 blanks (Schertz and others, 1994; QW85_07) at the Denver Central Lab. The source was believed to be the tablet form of mercuric chloride preservative. High concentrations of Kjeldahl nitrogen at western NASQAN stations served by the Denver laboratory during the early 1980's (Alexander and others, 1993) may relate, in part, to this bias. 10-01-91 Kjeldahl nitrogen "micro" method implemented (Jirka and others, 1976) with blank correction. Positive bias present in previous method no longer detected. Phosphorus 10-01-73 - Total phosphorus--Incomplete digestion in 04-30-90 the potassium persulfate method produced negatively biased concentrations (QW92_10). 01-01-79 - Dissolved phosphorus--Evidence of occasional 12-31-81 periods of positive bias based on reference sample measurements at the Denver Central Laboratory (Alexander and others, 1993) 05-01-90 - Total phosphorus--Dilution procedure 09-30-91 implemented with existing potassium persulfate method (QW92_10). Less bias observed for this method; the method may yield higher concentrations than previous method (greater than or equal to 0.01 mg/L) for samples with with suspended-sediment concentrations above 50 mg/L. 10-01-91 Total phosphorus--Kjeldahl "micro" method implemented (QW92_10). Comparative studies with the potassium persulfate method indicated that the analytical results of the new method did not display the negative bias of the old method; concentrations of the new method are likely to exceed those of the old method by more than 0.01 mg/L. Trace Before 1975 Selenium--The colorimetric diaminobenzidine elements method may have produced a positive bias as large as 5 ug/L (QW81_12). mid-1980s Arsenic--A change in the rounding algorithm increased the frequency of nondetected values after this time. Values reported as 1.0 ug/L prior to mid-1980s were reported as less than 1.0 ug/L after this time. _____________________________________________________________________________ revised 01/15/97