e., sample solution with no added indicator) www.selleckchem.com/HSP-90.html was equilibrated to the desired temperature, and a blank absorption spectrum was obtained. Indicator was then added (20 μL of 10 mM CR or 30 μL of 10 mM mCP, for a final concentration of 2 or 3 μM), and an absorbance spectrum of the colored, well-mixed sample was obtained. For all pH measurements,

absorbances were recorded at six or more wavelengths: the H2I, HI−, and I2 − absorbance maxima; the H2I/HI− and HI−/I2 − isosbestic wavelengths; and a non-absorbing wavelength. Absorbance at the non-absorbing wavelength was measured to confirm that the sample cell did not shift in the cell holder during the experiments. Wavelength resolution was 0.1 nm. Isosbestic wavelengths were determined as a function of temperature by titrating 0.7 M NaCl solutions with HCl at high pH (pH near 8) to obtain the HI−/I2 − isosbestic point; low-pH solutions (pH near 2) were titrated to obtain the H2I/HI− isosbestic

point. The amounts of added HCl were determined gravimetrically, and absorbance measurements were corrected for dilution. The e3/e2 term in Eq.  (2) was obtained by determining the molar absorptivity ratio 433εI/573εI of CR at pH = 12, where the I2 − form of the dye is highly dominant. In seawater of this pH, precipitation of magnesium and sulfate salts occurs. Therefore, a modified synthetic seawater (i.e., a solution containing salts of NaCl, KCl, and CaCl2) Alpelisib concentration was prepared wherein MgCl2 was replaced with CaCl2, and Na2SO4 was replaced with NaCl. Sodium hydroxide (0.01 m) was added to the modified synthetic seawater to raise the pH to 12. Absorbance measurements were made over a range of salinities Farnesyltransferase (20 ≤ S ≤ 40) and temperatures (278.20 ≤ T ≤ 308.22). Combining the e2 term with the K2T term produces an equation (i.e. Eq.  (2)) with fewer measured parameters ( Liu et al., 2011) and obviates the need for direct determinations of e2. To determine the − log(K2Te2) term of Eq.  (2), sample solutions were characterized using paired mCP and CR absorbance measurements over a range of temperatures and salinities. For each sample, solution pH was first determined using mCP absorbance ratios

(RmCP) at a known T and S ( Liu et al., 2011). In another aliquot of the same sample (same pH, T, and S), cresol red absorbance ratios (RCR) were then measured. The sample solutions consisted of tris-buffered synthetic seawater prepared gravimetrically; 0.06 m HCl was added to 0.08 mol of tris to achieve a 1:3 molal ratio of tris:tris–HCl. Reagent amounts and weights were specified via a spreadsheet provided by Dr. Andrew Dickson of UCSD-SIO. The spreadsheet calculates required amounts of salts to be added based on the amount of added HCl for each salinity and buffer ratio. This buffer ratio differs from the typical 0.04 m equimolal tris buffer preparation (DelValls and Dickson, 1998) in order to achieve CR absorbance ratios in the range 1.088 ≤ RCR ≤ 4.707 and mCP absorbance ratios in the range 0.494 ≤ RmCP ≤ 2.