Flavien Berwick flavienbwk

## Max_Dissolved_Oxigen.c
// --------- Max Dissolved Oxigen Saturation ------------//
//
// Equation for the Henry coefficient as a function of temperature and salinity is used to calculate values
// for unit standard atmospheric concentrations (USAC) in freshwater and seawater in equilibrium with air at a total pressure
// of 1 atmosphere. It is estimated that the possible error in the new USAC values is no greater than $\pm 0.1%$ and probably less.
// Tables and equations are presented for obtaining accurate USAC values in the ranges $0^\circ < t < 40^\cir C and 0 < S < 40$.
// Simple procedures are given for calculating standard atmospheric concentrations at pressures different from 1 atm.
//
// Reference https://water.usgs.gov/software/DOTABLES/
// Dissolved oxygen (DO) solubility over a range of user-specified values for
	// --------- Max Dissolved Oxigen Saturation ------------//
	//
	// Equation for the Henry coefficient as a function of temperature and salinity is used to calculate values
	// for unit standard atmospheric concentrations (USAC) in freshwater and seawater in equilibrium with air at a total pressure
	// of 1 atmosphere. It is estimated that the possible error in the new USAC values is no greater than $\pm 0.1%$ and probably less.
	// Tables and equations are presented for obtaining accurate USAC values in the ranges $0^\circ < t < 40^\cir C and 0 < S < 40$.
	// Simple procedures are given for calculating standard atmospheric concentrations at pressures different from 1 atm.
	//
	// Reference https://water.usgs.gov/software/DOTABLES/
	// Dissolved oxygen (DO) solubility over a range of user-specified values for