DOI: 10.4231/y13t-6775
title: Water vapor stable isotope memory effects of common tubing materials

description: &lt;p&gt;Water molecules in vapor can exchange with gaseous water molecules sticking to surfaces of sampling tubing, and exchange rates are unique for each water isotopologue and tubing material. Therefore, water molecules on tubing walls take some time to reach isotopic equilibrium with a new vapor isotopic signal. This creates a memory effect observed as attenuation time for signal propagation in continuous stable water vapor isotope measurement systems. Tubing memory effects in &delta;D and &delta;&lt;sup&gt;18&lt;/sup&gt;O measurements can limit the ability to observe fast changes, and because &delta;D and &delta;&lt;sup&gt;18&lt;/sup&gt;O memory are not identical, this introduces transient deuterium excess (D-excess, defined as &delta;D &ndash; 8* &delta;&lt;sup&gt;18&lt;/sup&gt;O) artifacts in time-varying observations. A comprehensive performance comparison of commonly used tubing material water exchange properties in laser-based measurement systems has not been published to our knowledge. &lt;/p&gt;

&lt;p&gt;We compared how a large isotopic step change propagated through five commonly used tubing materials for water isotopic studies, PFA, FEP, PTFE, HDPE, and copper, at two different temperatures and an air flow rate of 0.635 L min&lt;sup&gt;-1&lt;/sup&gt; through approximately 100 feet (~30.5 m) of &frac14; in. (6.35 mm) outer diameter (OD) tubing. All commonly used tubing materials performed similarly to each other in terms of attenuation times, reaching &delta;&lt;sup&gt;18&lt;/sup&gt;O location adjusted &delta;D and &delta;&lt;sup&gt;18&lt;/sup&gt;O 95% completion in less than 45 seconds, with slight variations based on temperature. PFA does appear to perform slightly better than the other materials, though memory metric differences are small. A tubing material commonly used in the early 2000&rsquo;s but reported to have memory effects on &delta;D, Dekabon, was also tested at ambient temperature and changing humidities. Dekabon isotopic equilibrium was not reached until nearly an hour after source transition, much later than H&lt;sub&gt;2&lt;/sub&gt;O mixing ratios equilibrated. Bev-A-Line XX (used in some soil O&lt;sub&gt;2&lt;/sub&gt; and CO&lt;sub&gt;2&lt;/sub&gt; gas studies) was also tested at ambient temperature, but it did not approach isotopic equilibrium until after nearly six hours of testing. Therefore, we cannot recommend the use of Bev-A-Line XX or Dekabon in water vapor isotope applications. Source transition from heavy to light or light to heavy affected isotopic transition speed only in experiments where H&lt;sub&gt;2&lt;/sub&gt;O ppm&lt;sub&gt;v&lt;/sub&gt; was changing. While shorter tubing length and smaller inner diameters shortens the delay of signal propagation through the tubing, they didn&rsquo;t greatly change the attenuation curves under these conditions for the current commonly used tubing materials tested. However, in Dekabon, attenuation curves were greatly extended with increased tubing length. Our results show that the commonly used plastic tubing materials tested were not inferior to copper in terms of isotopic memory under these conditions, and they are easier to work with and are less expensive than copper.  &lt;/p&gt;

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description: A laboratory experiment testing the water vapor isotopic memory of a few common air intake tubing materials (PFA, FEP, PTFE, HDPE, and copper, plus Dekabon and Bev-A-Line XX). Memory metrics for common materials are quantified at 2 different temperatures.