4.7 Article

Visualization of critical metals in marine nodules by rapid and high-resolution LA-ICP-TOFMS mapping

Journal

ORE GEOLOGY REVIEWS
Volume 154, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.oregeorev.2023.105342

Keywords

Polymetallic nodules; LA-ICP-TOFMS; Element mapping; High resolution; Critical metals

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Polymetallic nodules are widely distributed in the deep sea and contain important critical metals. Analyzing their trace elements can provide valuable information about source-to-sink processes and metal enrichment regimes. Element imaging is a useful technique for understanding the distribution of multiple elements, but traditional methods have limitations in terms of time and resolution. In this study, a new technique combining laser ablation with inductively coupled plasma time-of-flight mass spectrometry (LA-ICP-TOFMS) was used to map the distribution of elements in polymetallic nodules, demonstrating its feasibility and advantages over traditional methods.
Polymetallic nodules are one of the most ubiquitous critical metal reservoirs in the deep sea during early diagenesis. Trace elements including REY (Rare earth elements + Y), can provide a wealth of information to document the source-to-sink (STS) processes and critical metals enrichment regimes. Element imaging is an important see-through technique to display the distribution of multi-elements to understand the respective concentration relationship. However, traditional elemental mapping of macro (several millimeters) and micro (tens of micrometers) areas has remained a major challenge due to the long analytical time and low lateral resolution. Here, we apply inductively coupled plasma time-of-flight mass spectrometry (ICP-TOFMS), coupled to laser ablation (LA) with a low-dispersion two-volume sample cell and a dual concentric injector at both the macro-and micro-scales. LA-ICP-TOFMS mapping was applied to an entire polymetallic nodule (size of 10 * 9 mm2 @ 40 mu m2 spot size, 1300 mu m/s scan speed and 15 Hz frequency) and microdomains with microlayers (size of 700 * 350 mu m2 @ 1 mu m2, 200 mu m/s and 200 Hz), respectively. The intra-nodule distribution patterns of ele-ments are mainly controlled by the occurrence minerals. For example, the distribution patterns of some metals (e. g., Cu, Co, Ni) are similar to that of Mn, indicating these metals host in Mn-phase minerals. There is a trend of decreasing and then increasing of these elements from the inner to the outer layer, suggesting that the redox environment may have undergone a process from oxic to suboxic and then to oxic during the growth process. Our results demonstrate the feasibility of LA-ICP-TOFMS analysis on soft and porous materials, whose advantages include a shorter time and higher lateral resolution compared with traditional LA-ICP-QMS, expanding the geochemical mapping techniques for deep-sea early diagenetic sediments samples.

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