Water Resources Division (WRD) Policy on Publication of Sediment Size Data Determined by use of the Sedigraph In Reply Refer To: January 29, 1993 Mail Stop 415 OFFICE OF SURFACE WATER TECHNICAL MEMORANDUM NO. 93.11 Subject: Water Resources Division (WRD) Policy on Publication of Sediment Size Data Determined by use of the Sedigraph BACKGROUND The Water Resources Division has traditionally published only sediment fall diameter data which have been determined by the visual-accumulation tube, pipet, bottom withdrawal tube, or hydrometer. The Sedigraph is a much faster and cheaper method for size analysis and the Sediment Action Committee has recommended that it be approved as an alternative method of analysis for fall diameter. A comparison of pipet and Sedigraph methods has been documented in a memorandum from the Branch of Quality Assurance to the Office of Surface Water (OSW) dated December 14, 1992. For sizes in the silt-clay range, there is a general tendency for the Sedigraph to indicate about 5 to 10 percent more material is finer than a given size than indicated by the pipet method. For a given field site, comparison tests indicate that the relationship between sedigraph and pipet methods can be established by performing duplicate analyses. POLICY It is WRD policy that the Sedigraph is an approved method of analysis for fall diameter. Data produced using the sedigraph may be included in the WATSTORE System and published in the annual report provided the method of analysis is identified. Each District that chooses to use the Sedigraph method should perform duplicate sample analyses on at least 10 percent of the samples until the relationship between the Sedigraph and pipet results can be quantified for the site at which the sediment samples were collected. All future entries to WATSTORE are to include a method code to identify the type of analysis. The existing method code system in the QWDATA data structure is currently used by the National Water Quality Laboratory to indicate the method of analysis. Table 1 gives the method codes that identify the types of analysis used to determine sediment size. The codes D & W are only to be used for the sieve analyses, the codes V, S, P, B, & H are only to be used for the fall diameter determinations, and the codes C & M are only to be used to identify the direct measurement of particle size. The OSW encourages Sediment Laboratories to offer a silt-clay split as an alternative to the complete size analysis of the fine material. The percent clay can be entered as the fall diameter less than 0.004 mm with the appropriate method code. The method codes are not picked up by the tabling programs in NWIS-I. As with all water-quality data, this means that each table may display data that have been determined by different methods. Data produced by various methods can be identified by sorting the data by the method of analysis code. Method codes for historical data may be entered at the discretion of the individual District. Table 1. Method codes to be used to identify the type of laboratory analysis used for sediment size analysis. Method CODE METHOD C Measurement, direct (particle count) M Measurement, direct (optical) D Dry sieve W Wet sieve V V A tube S Sedigraph P Pipet B B W tube H Hydrometer Charles W. Boning, Chief Office of Surface Water This memorandum does not supersede any previous memorandums. DISTRIBUTION: A, B, FO, PO