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Marine Icing and Anti/De-icing Systems

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Marine Icing and Anti/De-icing Systems

Abstract

Shipping operations are on the rise in the Arctic region. Due to these increased activities, maritime transport operations are encountering significant challenges with respect to the safety and reliability. These shipping operations are comprised of commercial vessels such as oil tankers, container ships, fishing vessels, tourism cruises, research and offshore exploration vessels and icebreakers

In this work, an effort is being made to review icing phenomenon in the marine operations. Two primary sources of icing are focused namely: atmospheric and sea spray. It is found from the literature that sea spray icing is the main contributor towards the marine icing. This work discusses the available ice accretion prediction models on the ship and offshore structures. This work also reviews the anti/de-icing technologies that can be implemented on ships for operations in cold climate region. The significance of ice detection is acknowledged, and a brief review of various ice detection technologies is discussed

.

Liquid Water Content (LWC) Correlations

T. Rashid, H. Khawaja, K. Edvardsen

UIT The Arctic University of Norway, Tromsø, Norway

Conclusion

Cold Climate operations has increased due to various interests in the region. Severe ice accretion phenomenon is a challenge in cold climate region. The challenge can be encountered during marine operations, mainly caused by sea spray and atmospheric factors. The ice removal on the marine platforms is suggested to be achieved through suitable combination of ice detection and de/anti-icing methods.

Contact T. Rashid

Researcher,

University of Tromsø, Tromsø, Norway

E-mail:

taimur.rashid@uit.no

Marine Icing Phenomenon

MULTIPHYSICS 2015

LWC correlations contributing to Icing Sea Spray Icing

Icing Source

Droplet diameter Range (μm)

Mean droplet Diameter

(μm)

Liquid water Content

(g/m

3

)

Droplet

concentration (droplets per cm

3

) Breaking Waves

Wave Crests

1000 – 3500 60 – 1000

2400 150 -200

4600

Fog:

Advection Radiation Convection

6 - 64 4 - 36

~ 120

20 10 46

0.17 0.11 0.13

40 200 Clouds:

Stratus Cumulus

1.5 – 43 4 - 200

4.9 40

0.05 – 0.25

2.5 72

Droplets Characteristics of Various Icing Sources

LWC Correlation Correlation Variables

𝑤𝑤 = 𝑤𝑤

𝑜𝑜

𝐻𝐻

𝑠𝑠

𝑣𝑣

𝑟𝑟2

𝑒𝑒

−0.55ℎ

𝑤𝑤 is LWC of spray cloud (Kg/m

3

)

𝑤𝑤𝑤 is averaged LWC of spray cloud (Kg/m

3

) 𝐻𝐻

𝑠𝑠

is significant wave height (m)

𝑧𝑧 is spray cloud elevation above mean sea level (m) ℎ is elevation above the vessel deck (m)

𝐻𝐻

𝑟𝑟𝑟𝑟𝑠𝑠

root mean square wave height (m)

𝑧𝑧𝑧 is spray cloud elevation above wave wash zone (m) 𝑣𝑣

𝑟𝑟

is ship speed relative to incoming wave (m/s)

𝑤𝑤

𝑜𝑜

= 6.36𝑥𝑥10

−5

(empirical constant) 𝑤𝑤

𝑜𝑜

= 1.3715𝑥𝑥 10

−3

(empirical constant) 𝑤𝑤 = 𝑤𝑤

𝑜𝑜

𝐻𝐻

𝑠𝑠2.5

𝑒𝑒

−0.55ℎ

𝑤𝑤 = 1.35𝐻𝐻

𝑠𝑠2

𝑒𝑒

−0.53𝑧𝑧

𝑤𝑤

= 1.7𝑥𝑥 10

−4

𝐻𝐻

𝑠𝑠

𝑤𝑤𝑤 = 10

−3

𝐻𝐻

𝑠𝑠

𝑤𝑤 = 0.1𝐻𝐻

𝑠𝑠

𝑒𝑒

𝐻𝐻𝑠𝑠−2𝑧𝑧

𝑤𝑤 = 4.6𝑒𝑒

− 2𝑧𝑧𝐻𝐻𝑟𝑟𝑟𝑟𝑠𝑠

2

Anti De-Icing Methods

Chemical Thermal

Mechanical

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