Abstract

Manganese crusts (Mn-crusts) are a type of mineral deposit that exists on the surface of seamounts and guyots at depths of >800 m. We have developed a method to efficiently map their distribution using data collected by autonomous underwater vehicles and remotely operated vehicles. Volumetric measurements of Mn-crusts are made using a high-frequency subsurface sonar and a 3-D visual mapping instrument mounted on these vehicles. We developed an algorithm to estimate Mn-crust distribution by combining continuous subsurface thickness measurements with the exposed surface area identified in 3-D maps. This is applied to data collected from three expeditions at Takuyo Daigo seamount at depths of ∼1400 m. The transects add to ∼11 km in length with 12 510 m2 mapped. The results show that 52% of the surveyed area is covered by Mn-crusts with a mean thickness of 69.6 mm. The mean Mn-crust occurrence is 69.6 kg/m2 with a maximum of 204 kg/m2 in the mapped region. The results are consistent with estimates made from samples retrieved from the area, showing more detailed distribution patterns and having significantly lower uncertainty bounds for regional-scale Mn-crust inventory estimation.

Highlights

  • C OBALT-RICH manganese crusts (Mn-crusts) form on the slopes and shoulders of seamounts and guyots in geologically stable regions

  • While previous work analyzed small volumes of remotely operated vehicles (ROVs) data, the majority of data in this article have been collected using an autonomous underwater vehicles (AUVs), described in [26], with modifications made to the data acquisition system

  • As the AUV moves, these points will come in the illuminated region of the image; the RGB color values of the point can be identified based on the motion of the AUV

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Summary

INTRODUCTION

C OBALT-RICH manganese crusts (Mn-crusts) form on the slopes and shoulders of seamounts and guyots in geologically stable regions. This article presents a scalable way to determine the continuous mass distribution of Mn-crust over hectare-scale regions of the seafloor using visual and acoustic sensors This builds on the work described in [19], describing modifications to the data acquisition hardware, and presenting novel data processing methods that scale to the hectare-scale regions surveyed using this system. While previous work analyzed small volumes of ROV data, the majority of data in this article have been collected using an AUV, described in [26], with modifications made to the data acquisition system This includes real-time control of a double-gimbal system that orients the acoustic probe to be normal to the seafloor by analyzing the 3-D visual mapping data [27]. The advances in the sensor, platform, and novel algorithms described in this article allow estimates of Mn-crusts to be made over hectare-scale regions of the seafloor for the first time

AUV BOSS-A
Data Analysis Workflow
Seafloor Classification
Acoustic Data Interpretation
Data Fusion and Crust Volume Estimation
Continuous Flat Mn-Crust Deposits
Sediment to Nodules Transition
Sediment-Covered Flat Mn-Crust Near a Ledge
Compiled Results From All Dives
Discussion
Findings
CONCLUSION
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