Note – Fees are inclusive of d13C measurements, quality assurance reports, and 24/7 web access to past results and pending analyses. DOC extraction fee applies in addition to the standard price. Additional fee is charged if Oxygen-18 and Deuterium stable isotope measurements are requested.
We are a NATURAL Level 14C dating laboratory and cannot accept water samples that have been collected from any area that is near to a nuclear power plant, commercial or medical reactors, industrial/medical waste disposal sites or from within their drainage areas. The water samples must not be stored or handled in any laboratory or area that uses OR has ever used biomedical or artificially labeled 14C at any time.
Should you suspect that your samples may in any way have elevated 14C activities above peak Bomb Carbon levels (~200 pMC / 2.0 F14C), please DO NOT send the samples for testing. Water samples that produce activities above 200 pMC will incur extensive costs related to any cleanup necessary, equipment replacement and duplicate analyses required for other samples. These costs could easily run into the tens of thousands of dollars which you will be responsible for as the submitter.
Thoroughly flush the bottle with the sample at least 2 times before collecting the final sample with the aid of a water filter. Use a filter with pore sizes between 0.2-0.7 μm. If samples are not filtered, the DOC signature is at risk of changing while the samples are in transit.
Fill the bottle with as little headspace as possible.
If samples are to be stored for any length of time, they must be refrigerated between 3-5˚C (37-41˚F).
Seal the space between the bottle and the cap with tape to prevent carbon dioxide (CO2) exchange with the atmosphere during shipment.
If possible, samples should be sent chilled or cold (NOT frozen). First-aid ice packs work well for this purpose; they will ensure that samples do not heat up too much while in transit.
Before placing into a cooler or cardboard box, the bottles should be placed inside a plastic bag and sealed. Please use shipping containers with enough packing material to prevent breakage.
NOTE: Beta Analytic WILL NOT return water samples, bottles or coolers.
We recommend commercial courier or registered first-class mail when sending the samples to the lab. Please email the courier name and tracking number so we can monitor your package.
Dissolved organic carbon (DOC) is the largest pool of organic matter and reduced carbon in the oceans, roughly equal in size to CO2 in the atmosphere (Beaupré 2007). DOC is also found in terrestrial ecosystems and plays an important role in the global carbon cycle, partially due to its ability to transport carbon between different pools in the ecosystem (Kolka 2008). DOC can be sourced from outside the ecosystem (atmospheric carbon, long distance transport) or within the ecosystem (plants/microbial or from soils/sediments), and higher levels of organic material are not uncommon in environments with lower oxygen levels such as swamps (Bruckner 2016).
The measurement of radiocarbon in DOC is a useful tool for identifying the sources and cycling processes of DOC in natural waters, both in freshwater and marine (Xue 2015). While the absolute ages alone can provide information on the sources of the carbon contained in the DOC, it is most useful when combined with additional information, such as 13C measurements or other stable isotope measurements from nutrients such as phosphate or nitrate. This is due to the role of DOC in nutrient cycling and availability in ecosystems.
Along with other nutrients present in the ecosystem, radiocarbon and stable isotope measurements of DOC allow for a more complete picture of an ecosystem’s health. When samples are collected along a transect in a watershed, agricultural area, etc., the data can be used to quantify contributions to the DOC pool from both old and modern carbon sources, determine water quality, and ultimately determine the impact on a particular ecosystem. As an example, a pristine, low-impacted area in the Florida Everglades will have a modern or near-modern radiocarbon age, indicating a relatively low contribution from “old” carbon sources like peat deposits and high contributions from modern sources, primarily CO2 uptake by native wetland C3-plants of atmospheric CO2 (Stern 2007).