Overview

The Chemistry laboratory is used by shipboard scientists to conduct organic and inorganic geochemical analyses. A primary responsibility of the organic geochemists is to provide hydrocarbon data for safety and environmental concerns. In addition, instruments are available for determining the source, amount, and maturity of organic matter; carbonate content; and total carbon, nitrogen, and sulfur.

Inorganic geochemists have a wide array of analytical instruments at their disposal for determination of a large range of interstitial water constituents that typically include pH, alkalinity, chloride, calcium, magnesium, sulfate, potassium, strontium, sodium, manganese, phosphate, silica, and ammonium. Two Laboratory specialists provide dedicated, 24-hour technical support.

Organic Geochemistry

Safety Monitoring

Organic geochemists perform a vital function on the ship by providing routine safety monitoring for hydrocarbon gases. Typically, a ~5 cm³ sediment headspace sample is collected at a frequency of one every 10 meters, heated, and the evolved gases are analyzed with a gas chromatograph (GC). When gas pockets are detected in the core liner, a vacutainer sample can be taken to sample the gas directly. One Agilent GC is equipped with an FID detector for rapid determination of methane, ethane, ethylene, propane, and propylene. The second Agilent GC is equipped with FID and TCD detectors to measure hydrocarbons from methane to hexane. In addition, nonhydrocarbon gases such as hydrogen sulfide, oxygen, nitrogen, carbon dioxide, and carbon monoxide can be analyzed at the same time as hydrocarbon gases.

Guidelines for this responsibility can be found at these links:

ODP Technical Note 30

http://www-odp.tamu.edu/publications/tnotes/tn30/INDEX.HTM

EPSP Safety Review Report and Expedition Safety Package Guidelines

https://www.iodp.org/top-resources/program-documents/policies-and-guidelines/1178-epsp-safety-review-report-guidelines-may-2022/file

Organic Matter

A Weatherford Instruments Source Rock Analyzer (SRA) uses a pyrolysis technique to identify the type and maturity of organic matter.

Elemental Analysis

Sediment samples can also be analyzed for total carbon, nitrogen, sulfur, and carbonate carbon. The total organic carbon of the sediment can be determined by calculating the difference between total carbon and carbonate carbon. Carbonate carbon is measured by coulometric titration using a Coulometrics CM5011 analyzer. A Thermo Electron Flash EA 1112 Elemental Analyzer is used to determine total carbon, nitrogen, and sulfur.

Inorganic Geochemistry

Shipboard interstitial (pore) water analyses are typically performed on waters extracted from 5–10 cm whole-round sections. The routine shipboard interstitial water sampling program calls for one whole-round sample to be taken per core for the first six cores, and one sample every third core thereafter. Pore water is extracted from core samples by applying pressures up to 40,000 lb (~4150 psi) with a Carver hydraulic press. Immediately after extraction and filtration, aliquots are analyzed for salinity using a hand-held particular refractometer and for pH and alkalinity using Metrohm titrators.

Chloride is also determined by titration. A variety of nutrients and other pore water constituents (e.g., ammonium, silica, phosphate, nitrate, and nitrite) can be determined using a Cary UV-VIS spectrometer. Numerous cations and anions can be analyzed using a Metrohm Ion Chromatograph (e.g., calcium, magnesium, sulfate). A variety of other elements can be determined by inductively-coupled plasma optical emission spectrometry on a Agilent ICP-OES 5110. A typical suite of elements determined for interstitial water samples includes Sr, Li, Fe, Mn, B, and Ba. In addition, hard rock samples can be analyzed for all major and minor elements.