o_to_sal: Convert Oxygen isotope ratio to salinity

In ctdenney/OGFLtools: Several utility functions for use in the OGFL

Convert Oxygen isotope ratio to salinity

Description

This function uses published relationships of d18O and environmental salinity from either Ingram et al(1996) or McLaughlin et al(2006) to calculate salinity when given d18O. It is specific to the San Francisco Estuary.

Usage

o_to_sal(d18O, source)

Arguments

d18O	is the measured d18O
source	is the desired source function. Currently only 'ingram' and 'mclg' are supported.

References

Ingram BL, Conrad ME, Ingle JC. Stable isotope and salinity systematics in estuarine waters and carbonates: San Francisco Bay. Geochim Cosmochim Acta. 1996;60(3):455‐467. https://doi.org/10.1016/0016‐ 7037(95)00398‐3 McLaughlin K, Kendall C, Silva SR, Young M, Paytan A. Phosphate oxygen isotope ratios as a tracer for sources and cycling of phosphate in North San Francisco Bay, California. J Geophys Res Biogeo. 2006;111(3):1‐12. https://doi.org/10.1029/2005JG000079

Examples

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ctdenney/OGFLtools documentation built on Feb. 8, 2023, 5:47 p.m.