Improved throughput for δ18O and δD measurements of water with Cavity Ring-Down Spectroscopy

Author(s):  
Magdalena E. G. Hofmann ◽  
Zhiwei Lin ◽  
Jan Woźniak ◽  
Keren Drori

<p>Oxygen (<sup>18</sup>O/<sup>16</sup>O) and deuterium (D/H) isotopes are a widespread tool to trace physical and chemical processes in hydrology and biogeosciences. Precision and throughput are key parameters for water isotope analysis. Here, we will present two new methodologies for the Picarro L2130-i Cavity Ring-Down Spectroscopy (CRDS) water isotope analyzer that allow to increase the throughput with no compromise of data quality.</p><p>The Picarro Express Method now distinguishes between a memory reduction stage and a sample analysis stage and allows to measure up to 50 samples per day while maintaining the excellent precision of CRDS (i.e. 0.01‰ for δ<sup>18</sup>O and 0.05‰ for δD). This corresponds to doubling the throughput compared to the standard Picarro methodology. The Picarro Survey Method makes use of ultrafast injections and sorts the samples by their measured isotopic values, enabling a powerful new strategy to reduce memory effects.</p><p>We will discuss different measurement strategies to increase the throughput for routine water isotope analysis. The improved methodologies do not require any hardware changes and are solely based on modifications of the injection procedure. If you are interested in Picarro’s off-the-shelve solution for increasing productivity of your existing and future installations, please visit the Picarro vEGU 2021 booth for a free voucher.</p>

2009 ◽  
Author(s):  
K. Hiromoto ◽  
H. Tomita ◽  
K. Watanabe ◽  
J. Kawarabayashi ◽  
T. Iguchi ◽  
...  

2016 ◽  
Vol 99 (sp1) ◽  
pp. 177-184 ◽  
Author(s):  
Rebecca Hood-Nowotny ◽  
Leo Mayr ◽  
Nabil Saad ◽  
Rakesh K. Seth ◽  
Goggy Davidowitz ◽  
...  

2020 ◽  
Author(s):  
Magdalena E. G. Hofmann ◽  
Zhiwei Lin ◽  
Thomas Doherty ◽  
Jonathan D. Bent ◽  
Gregor Lucic

<p>Triple oxygen isotope data (denoted as <sup>17</sup>O-excess) have been used to constrain meteorological processes, plant fractionation processes, animal metabolism, and a variety of other physical and chemical processes. Measurement precision is key in order to successfully apply this promising new tracer to a range of scientific questions. Up to date, the highest measurement precision for <sup>17</sup>O-excess on water was achieved by converting water to O<sub>2</sub> and subsequent mass spectrometric analysis of O<sub>2</sub> (Barkan and Luz, 2005). This approach allows to reach a measurement precision of about 5-6permeg. However, it is very difficut to setup and only a few laboratories worldwide succesfully use this methodology. A far simpler approach is to use Cavity Ring-Down Spectroscopy (CRDS), i.e. the Picarro L2140-i analyzer that measures δ<sup>18</sup>O, δ<sup>17</sup>O, δD and determines <sup>17</sup>O-excess. To date, the <sup>17</sup>O-excess measurement precision of CRDS was limited to 10-15permeg. Here, we will present a new metholodology that allows to reach a similar or even better precision compared to the mass spectrometric approach. The improved methodology does not require any hardware changes but is solely based on modifications of the injection procedure. </p>


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