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Recovery of a Lost Subsea Asset at Full Ocean Depth in the Mariana Trench (10,925 m ± 4) Using a Crewed Submersible

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In 2019, the Deep Submergence Support Vessel Pressure Drop embarked on the third leg of the Five Deeps Expedition. Over the course of 10 days, the full ocean depth submersible Deep Submergence Vehicle Limiting Factor made a record five dives to the bottom of the Mariana Trench: four to the Challenger Deep, one to the Sirena Deep. The submersible was supported by three scientific landers, one of which became stuck on the seafloor at 10,925 m depth. Here we describe how, during the third dive of the campaign, the expedition utilized the submersible to rescue this lost asset from full ocean depth. The expedition was not only significant for its operational jump from single full ocean depth dives to multiple dives in a short space of time, but demonstrated that assets lost in the deepest 45% of the oceans are no longer irretrievable.
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TECHNICAL NOTE
Recovery of a Lost Subsea Asset at Full Ocean
Depth in the Mariana Trench (10,925 m ± 4)
Using a Crewed Submersible
AUTHORS
Alan J. Jamieson
Minderoo-UWA Deep-Sea Research
Centre, The University of Western
Australia
Patrick Lahey
Triton Submarines LLC,
Sebastian, Florida
Rob MacCallum
EYOS Expeditions, Isle of Man,
United Kingdom
Stuart Buckle
Tim Macdonald
Victor Vescovo
Caladan Oceanic LLC,
Southlake, Texas
ABSTRACT
In 2019, the Deep Submergence Support Vessel Pressure Drop embarked on
the third leg of the Five Deeps Expedition. Over the course of 10 days, the full
ocean depth submersible Deep Submergence Vehicle Limiting Factor made a re-
cord ve dives to the bottom of the Mariana Trench: four to the Challenger Deep,
one to the Sirena Deep. The submersible was supported by three scientic
landers, one of which became stuck on the seaoor at 10,925 m depth. Here
we describe how, during the third dive of the campaign, the expedition utilized
the submersible to rescue this lost asset from full ocean depth. The expedition
was not only signicant for its operational jump from single full ocean depth
dives to multiple dives in a short space of time, but demonstrated that assets
lost in the deepest 45% of the oceans are no longer irretrievable.
Keywords: submersible, lander, Mariana Trench, exploration, asset recovery
Introduction
T
he exploration of Earths marine
frontiers is fraught with challenges,
and perhaps none more so than reach-
ing the deepest parts of the oceans.
Challenges such as high hydrostatic
pressure and distance from the surface
make such endeavors infrequent and
very expensive. Decades ago, the
bathyscaphes Trieste and Archimede
proved that it could be done, al-
though the former only made one
trip to full ocean depth and the latter
did many very-deep dives but none to
the deepest points (Piccard & Dietz,
1961, and Jarry, 2003, respectively).
More recent human occupied vehicles
(HOVs) such as DeepSea Challenger
were successful in reaching full ocean
depth but did so only once (Gallo
et al., 2015). Remotely operated vehi-
cles such as Kaiko and Nereus also
reached full ocean depth but were sub-
sequently lost (Tashiro et al., 2004,
and Cressay, 2014, respectively). Cur-
rently, there are several HOVs capable
of diving to 6,5007,000 m such as
Alvin (United States; Piecuch 2021),
Shinkai 6500 (Japan; Komuku et al.,
2007), and Jiaolong (China; Liu
et al., 2010) and, more recently, the
deeper diving submersible Fendouzhe
has reached full ocean depth multiple
times (China; Liu et al., 2021).
In 2017, construction of a new
submersible began as a privately
funded joint project between Caladan
Oceanic LLC and Triton Submarines
LLC (Jamieson et al., 2019). The ob-
jective was to produce a fully certied
submersible capable of taking two
people repeatedly to full ocean
depth on an operational basis. The
HOV would be used in an expedi-
tion, known as Five Deeps,tovisit
the deepest point in every ocean:
The Puerto Rico Trench (Atlantic),
SouthSandwichTrench(Southern),
Java Trench (Indian), Mariana
Trench (Pacic), and the Molloy
Hole (Arctic), in that order (Stewart
& Jamieson, 2019; Jamieson, 2020).
During the expedition, the HOV
successfully completed this explora-
tion challenge as well as other ven-
tures such as tourism, marine
archaeology, and deep-sea science.
The expedition began in Decem-
ber 2018. Following 14 test dives
off the Bahamas, the submersible
achieved the rst of the ve deeps at
8,376 ± 5 m in the Puerto Rico
Trench on 19th December 2018
(Jamieson et al., 2020); followed by
the second at 7,434 ± 3 m in the
South Sandwich Trench, 3rd February
2019 (Jamieson et al., 2021); and the
third at 7,192 ± 5 m the Java Trench
on 5th April 2019 (Jamieson et al.,
2022). The expedition arrived at the
Winter 2023 Volume 57 Number 1 151
Mariana Trench on 26th April 2019,
and given the prestige of this location
and its extreme depth, a greater
amount of time (10 days) was allocated
to this site. The objectives were to
complete four dives, comprising two
single occupant solodives, a dive
for DNV-GL (Det Norske Veritas-
Germanischer Lloyd) classication,
and a dive for the submersible manu-
facturers. This many dives to full
ocean depth had never been attempted
before making it a highly ambitious
undertaking. Here, we describe the
achievement of more dives to Challeng-
er Deep in 10 days than were planned,
and how the HOV was used to suc-
cessfully locate and recover a lost lander
from the deepest point on Earth.
Material and Methods
The Deep Submergence Vehicle
(DSV) Limiting Factor or Triton
36,000/2 (Triton Submarines, United
States) is a full ocean depth rated two-
crewed submersible (Jamieson et al.,
2019) (Figure 1A). The submersible
is operated from the 68 m-long Deep
Submergence Support Vessel (DSSV)
Pressure Drop and supported by a
number of small surface craft and
three full ocean depth rated lander
systems (Figure 2B). The landers had
a footprint of 1 × 1.5 m and were
1.5 m high with a weight in water
of ~50 kg -ve. All these assets com-
bined are collectively known as the
Hadal Exploration System, operated
at the time by Caladan Oceanic Ltd
(United States).
DSV Limiting Factor communi-
cated with the ship, and the support-
ing landers via underwater modems
(GPM300 Acoustic Modem, L3 Oce-
ania,Fremantle,Australia).Video
data were acquired using three exter-
nally mounted high-denition video
cameras (IP Multi SeaCam 3105;
Deep Sea Power and Light, San
Diego, CA), illuminated by ten
15,500 lumen LED lights (LED-
1153-A3-SUS; Teledyne Bowtech,
Aberdeen, UK). Depth and tempera-
ture were recorded by twin Conduc-
tivity, Temperature, and Depth
(CTD) probes (SBE 49 FastCAT,
SeaBird Electronics, Bellevue, WA),
where depth was recorded with an ac-
curacy of 0.1%. It was also equipped
with a Raptorhydraulic manipu-
lator arm (Kraft TeleRobotics,
Overland Park, KS). The three iden-
tical landers were free-fall baited
camera landers primarily used for
scientic studies, equipped with the
same camera, lights, CTDs, and
underwater modems as Limiting Fac-
tor.BothLimiting Factor and the
landers descend to depth by virtue of
FIGURE 1
(A) The full ocean depth rated two-crewed submersible DSV Limiting Factor, and (B) one of the
supporting landers (Skaff). The Limiting Factor image was taken by Skaff at 10,920 m in Chal-
lenger Deep, and the Skaff image was taken by the Limiting Factor at 3,000 m in the Puerto Rico
Trench.
FIGURE 2
Images from the lost lander Skaff at 10,925 m, showing (A) Closp landing in the distance, (B)
the submersible arriving at Closp, (C) the submersible approaching the lost lander, and (D) the
submersiblelander rendezvous. The bait arm bars in (D) are 50 cm apart.
152 Marine Technology Society Journal
expendable ballast weights, which
when released via the modems or
back-up burn-wire timers (landers) or
manually (on board the HOV) return
the vehicles to the surface via positively
buoyant syntactic foam (TG39/
11,500, Trelleborg Applied Technolo-
gies, Rochdale, UK). Recovery on the
surface was aided by Iridium satellite
beacons (iBCN, Novatech, Canada)
and Xenon strobes (MMF-7500,
Novatech, Canada).
Prior to launching the HOV, the
DSSV Pressure Drop mapped pro-
posed dive sites and surrounding
areas in the Mariana Trench using a
hull-mounted EM 124 multibeam
echosounder (MBES; Kongsberg,
Norway; see Bongiovanni et al.,
2022). The three landers were then
deployed between 1 and 2 km apart,
and their positions triangulated using
modems operated from the ship and
one of its supporting surface boats.
Limiting Factor was then deployed,
using one of the landers as a marker
to aim for where the MBES data
identied as the deepest point.
Results
Following the rst dive by Limit-
ing Factor to 10,924 m on the 28
th
April 2018, a second solo dive was
undertaken on the 1
st
of May. The
landers Skaff, Closp, and Flere were
deployed prior to this second dive to
depths of 10,925, 10,912, and
10,877 m, respectively. On arrival
on the sea oor, Limiting Factor ren-
dezvoused with Skaff that had been de-
ployed at 11.3700° N/142.5883° E. It
became apparent that the lander was
leaning forward into very soft sediment
that buried the entire 1-m-long bait
arm and had accumulated across the
base of the lander. It was not recog-
nized at the time that this partial burial
may be problematic. However, follow-
ing the surfacing of the HOV, acoustic
release commands were transmitted
from the ship to all the landers. Closp
and Flere surfaced on time, yet Skaff
did not, despite both the primary
and back-up burn wire releases having
activated. Following a period whereby
a back-up timed release should have
released the ballast weight, it was ap-
parent that Skaff was indeed stuck on
the seaoor.
The following day, it was decided
to make the third dive an attempt to
rescue the lander. The lost lander had
a value of $250,000, but it was also
the only lander that had been tted
with a $150,000 special issue
Omega Seamaster Planet Ocean Ultra
Deep model.
On May 3
rd
,Closp was deployed
aiming for exactly the same position
as Skaff to act as a navigation beacon
for the submersible. To prevent Closp
also becoming stuck in the soft sedi-
ments, the ballast weight was tethered
1 m below the main frame so that no
part of the lander was itself in contact
with the seaoor.
In the period between the sub-
mersible leaving Skaff on the 1
st
to
the rescue attempt on the 3
rd
, the bat-
tery power on the lander had reduced.
This resulted in the camera still re-
cording, but the light had since failed.
Fortuitously, this allowed Skaff to re-
cord the rescue in greater detail than
if the light had been on, and further-
more, the camera was facing toward
Closp and actually recorded the land-
ing at an estimated distance of ~200
m (Figure 2A).
Nearly 5 hr after Closp landed, the
arrival of Limiting Factor on the
sea oor was also lmed by Skaff
(Figure 2B) landing between 100
and 200 m from Closp.TheHOV
then spent 50 min making a slow ap-
proach to Skaff using the ashing
light of the recovery beacon to visu-
ally locate it (Figure 2C-D).
Upon nding Skaff, the submers-
ible did a 360° inspection of the
lander (Figure 3A), and it was decided
to use the manipulator arm to dis-
lodge the lander from the sediment
by simply pushing the lander at the
top of its frame in the opposite direction
FIGURE 3
Images from the submersible showing (A) rendezvousing with the lost lander Skaff, (B) Skaff
ascending off the seaoor after being stuck for over 2 days, (C) returning to Closp, and (D)
witnessing the ballast release and ascent of Closp.
Winter 2023 Volume 57 Number 1 153
to which it was leaning. This was
achieved within 12 min (Figure 3B),
and the lander then ascended toward
the surface as normal.
The Limiting Factor then navigat-
ed back to Closp and requested an
acoustic release command from the
surface (Figure 3C). The submersible
then waited to observe and conrm
Closp beginning its ascent from the
seaoor (Figure 3D) before returning
itself.
Two days later, the HOV and
supporting landers undertook a
fourth dive to Challenger Deep. The
expedition then relocated to eastward
to Sirena Deep and undertook a dive
to 10,705 m with the Limiting Factor
and the three landers, concluding the
Mariana Trench campaign of the Five
Deeps Expedition.
Discussion
The Mariana Trench campaign
was extraordinary for multiple rea-
sons. It rst demonstrated that a full
ocean depth HOV could be capable
of repeated dives to full ocean
depth. The dive that saw the rescue
of Skaff was also a certication dive
as the passenger in the sub at the
time was a DNV-GL inspector who,
upon returning, issued the Limiting
Factor with the rst ever classication
of unlimited depth.It also demon-
strated that, in the space of just 10
days, the whole systemfrom the
ship, multibeam, HOV, and landers
was capable of mapping the deepest
place on earth, diving 5 times in a
submersible and achieving 20 scien-
tic lander deployments between
2,100 and 10,900 m depth. It also
demonstrated the ability to locate
and rendezvous with landers pre-
deployed on the seaoorasthiswas
done on all ve dives on this cam-
paign, with two on the rescue
dive (Figure 3). This is a major oper-
ational jump from single dives to
multiple, and more complex dives
at full ocean depth. The lander res-
cue also shows that assets lost in
the deepest 45% of the oceans are
no longer irretrievable.
It is important to note that prior
to the Mariana Trench leg of the
Five Deeps Expedition, the submers-
ible had only completed four dives to
the maximum depth of trenches
greater than 6,000 m (the Puerto
Rico and South Sandwich trenches,
and two dives in the Java Trench).
The rst Java Trench dive was the
only time prior to the Mariana
Trench leg that the submersible
managed to rendezvous with a land-
er, making the rescue of Skaff at
10,925 m all the more challenging
and remarkable.
The DSV Limiting Factor has
since gone on to complete a total of
22 dives to Challenger Deep and Sire-
na Deep (including another full ocean
depth lander rescue at 10,688 m in
2021), as well as several other dives
to over 10,000 m (Tonga, Kermadec,
and Philippine trenches).
Acknowledgments
We thank the entire crew, compa-
ny, and sub team of the DSSV Pres-
sure Drop, including Commander
Don Walsh USN (Ret) and Paul
Henry Nargeolet.
Corresponding Author:
Alan J. Jamieson
Minderoo-UWA Deep-Sea Research
Centre,
The University of Western Australia
35 Stirling Highway, Perth, WA 6009
Email: Alan.j.jamieson@uwa.edu.au
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JIAOLONG's function and capability were fully tested during its 37 dives. The longest underwater time was 543 minutes, and the deepest dive of 3759 m was made on its 37th dive. The Chinese national flags and memorial "Dragon Palaces" were placed on the seafloor. 525 mL of pressure-sustained seawater and two sea cucumbers were sampled. Test results have indicated that all the functions and capabilities were in good agreement with the design data. © 2010 Science China Press and Springer-Verlag Berlin Heidelberg.
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The South Sandwich Trench is a 965 km long arcuate subduction trench spanning the South Atlantic and Southern oceans, isolated from most other hadal (areas where water depths exceed 6000 m) environments by thousands of kilometres. This feature represents the coldest known hadal ecosystem with ambient sub-zero temperatures recorded from bathyal depths to over 7000 m water depth. Very little research has been carried out into the hadal fauna of this trench since the Russian expeditions of the 1960s and 70s. Here, we report the first visual assessment of hadal fauna from the South Sandwich Trench from a series of seven baited camera and trap deployments between 6044 m and the deepest point at 8265 m water depth, a location called Meteor Deep. Three species of hadal fish (Liparidae), with very low population densities were observed at depths shallower than expected, likely due to the piezo-thermal effect decreasing their depth range. Four species of scavenging amphipods were recovered, extending the known distribution of Eurythenes andhakarae, Hirondellea dubia, and Bathycallisoma schellenbergi to the South Sandwich Trench. Large densities of brittle stars (Ophiuroidea) were seen in the shallower hadal depths, while dense aggregations of holothurians (Elpididae) were observed within trench-fill basins located along the deep trench axis coincident with a visible surficial layer of surface derived detritus. In addition, gastropods, sponges, and stalked crinoids were observed. Importantly, this study highlights the endemic community present at hadal depth within this somewhat unique high pressure-low temperature environment.
Article
The first direct observations of the diversity and density of benthic epifauna from hadal depths was reported in 1965 from depths of 7300 m in the Puerto Rico Trench. The most striking part of the report from was an account of observing 200 snailfish (Liparidae) during a one mile transect by the bathyscaphe Archimède - an extraordinarily high-density of fish for hadal depths. In 2019 the submersible DSV Limiting Factor revisited the exact same site in the Puerto Rico Trench. No snailfish were observed. However, a large number of the holothurian Peniagone sp. were seen in a density similar to that reported originally for the snailfish. The holothurian has a similar exterior colour, texture and morphology to the snailfish. It is concluded that the reported hadal snailfish of the Puerto Rico Trench was in fact a misidentification of the holothurian Peniagone sp.
Article
Full ocean depth exploration (depths of ~11,000 m) is still a rarity in deep-sea exploration. Following the 1960 Trieste dive to the Challenger Deep, it was 52 years before Deepsea Challenger followed suit. Between these dives, there was also the French bathyscaphe Archimède, operational in the 1960s, which performed a number of significantly deep dives. However, 7 years after the Deepsea Challenger , a new wave of full ocean depth dives have been undertaken in the DSV Limiting Factor , a new two-person full ocean depth submersible. Described herein is an update of the recent series of full ocean depth dives in the DSV Limiting Factor and a collation of all significantly deep dives and sub crew in full ocean depth submersibles. These historical dives are discussed, as well as the latest dives from the Five Deeps Expedition using the DSV Limiting Factor, within the context of and challenging the validity of common analogies with lunar exploration. This article aims to provide a little perspective and pride in full ocean depth exploration.