Salinity and total dissolved solids measurements for natural waters: An overview and a new salinity method based on specific conductance and water type

被引:17
|
作者
McCleskey, R. Blaine [1 ]
Cravotta, Charles A., III [2 ]
Miller, Matthew P. [1 ]
Tillman, Fred [3 ]
Stackelberg, Paul [4 ]
Knierim, Katherine J. [5 ]
Wise, Daniel R. [6 ]
机构
[1] US Geol Survey, 3215 Marine St,Suite E 127, Boulder, CO 80303 USA
[2] US Geol Survey, New Cumberland, PA 17070 USA
[3] US Geol Survey, 520 North Pk Ave, Tucson, AZ 85719 USA
[4] US Geol Survey, 425 Jordan Rd, Troy, NY 12180 USA
[5] US Geol Survey, 401 Hardin Rd, Little Rock, AR 72211 USA
[6] US Geol Survey, 601 SW 2nd Ave,Suite 1950, Portland, OR 97204 USA
关键词
Salinity; Total dissolved solids; TDS; Specific conductance; Geochemical codes; Proxy; Surrogate; ELECTRICAL-CONDUCTIVITY; UPPER COLORADO; SCALE; 1978; SALINIZATION; GROUNDWATER; BASEFLOW; STREAMS; RIVERS; FLUX;
D O I
10.1016/j.apgeochem.2023.105684
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The total concentration of dissolved constituents in water is routinely quantified by measurements of salinity or total dissolved solids (TDS). However, salinity and TDS are operationally defined by their analytical methods and are not equivalent for most waters. Furthermore, multiple methods are available to determine salinity and TDS, and these methods have inherent differences. TDS is defined as the mass of anhydrous residue remaining in a sample vessel after evaporation and subsequent oven drying at a defined temperature. Salinity is a measure of the mass of dissolved salts in a given mass of solution. In addition, there are approaches that quantify the total solute (TS) concentration, including gases. The purpose of this study is to develop a proxy method using specific conductance and major-ion water type to reliably predict salinity, TDS, and/or TS. Thus, we compared several methods to calculate salinity, TDS, and TS for 6391 surface water samples and conclude the following: TDS measurements are best suited for studies of anhydrous residue (e.g., evaporites); salinity determined by summing the speciated ion concentrations, termed S n-ary sumation spec, is the most comprehensive method to represent the concen-tration of dissolved constituents in natural waters; and TS determinations are useful if dissolved CO2 and other gases are of interest. Thus, we utilized S n-ary sumation spec to compare differences between the various salinity, TDS, and TS methods, and to develop a new proxy method to predict salinity based on specific conductance (SC) and major ion water type, termed SSC_WT. For the surface waters used in this study, the median difference between TDS and S n-ary sumation Spec was between-19% and-24%, depending on the method. The median difference between SSC_WT and S n-ary sumation Spec was-2.4% for the samples in this study. The SSC_WT approach is cost effective, rapid, and capable of providing reliable real-time salinity determinations at surface water sites where SC data are available and water type is known.
引用
收藏
页数:13
相关论文
共 11 条