Drone-Based Autonomous Robot Diagnostic System for Gas and Oil Pipelines in the Arctic and Far North

2018 ◽  
Vol 38 (9) ◽  
pp. 677-679 ◽  
Author(s):  
Yu. G. Kabaldin ◽  
D. A. Shatagin ◽  
A. V. Kiselev ◽  
M. V. Zhelonkin ◽  
A. A. Golovin
2018 ◽  
Vol 35 (4) ◽  
pp. 110-113
Author(s):  
V. A. Tupchienko ◽  
H. G. Imanova

The article deals with the problem of the development of the domestic nuclear icebreaker fleet in the context of the implementation of nuclear logistics in the Arctic. The paper analyzes the key achievements of the Russian nuclear industry, highlights the key areas of development of the nuclear sector in the Far North, and identifies aspects of the development of mechanisms to ensure access to energy on the basis of floating nuclear power units. It is found that Russia is currently a leader in the implementation of the nuclear aspect of foreign policy and in providing energy to the Arctic region.


Antiquity ◽  
2015 ◽  
Vol 89 (345) ◽  
pp. 740-742 ◽  
Author(s):  
Herbert Maschner

This review considers three books on the archaeology of territories situated around the Bering Sea—a region often referred to as Beringia, adopting the term created for the Late Pleistocene landscape that extended from north-east Asia, across the Bering Land Bridge, to approximately the Yukon Territory of Canada. This region is critical to the archaeology of the Arctic for two fundamental reasons. First, it is the gateway to the Americas, and was certainly the route by which the territory was colonised at the end of the last glaciation. Second, it is the place where the entire Aleut-Eskimo (Unangan, Yupik, Alutiiq, Inupiat and Inuit) phenomenon began, and every coastal culture from the far north Pacific, to Chukotka, to north Alaska, and to arctic Canada and Greenland, has its foundation in the cultural developments that occurred around the Bering Sea.


Nordlit ◽  
2012 ◽  
Vol 16 (1) ◽  
pp. 47 ◽  
Author(s):  
Einar-Arne Drivenes

The research and commercial activity in the Scandinavian portion of the Arctic increased appreciably in the last decades of the 19th century and up until the 1920s. Not unexpectedly, the idea arose during this period to bring the largest group of the as yet unclaimed Arctic islands, Spitsbergen, under Norwegian or Swedish control. Norwegian political ambitions in the far north seem to have expanded proportionally with economic and scientific activity. What role did science play in this process? In the contest to win Svalbard, Norwegian authorities deliberately used research results and research activity as justification that Spitsbergen was Norwegian. Also, Spitsbergen researchers worked systematically towards a Norwegian conquest of the archipelago, economic and cultural at first, but ultimately political.


2021 ◽  
Author(s):  
Veerendhar Ponagandla ◽  
Liangjian Liu ◽  
Duane DeGeer

Abstract Increasing demand for energy is driving the need to explore the deeper oceans and the far north. While higher temperature, pressure and longer tie-backs are challenges going deep, highly sensitive environment is an issue exploring far north. The discovery of large reserves in the far north has brought the challenges of exploration, production, and transportation in the cold regions like Prudhoe Bay, the Mackenzie Delta, and the Arctic Islands into focus. To transport hydrocarbons to market, pipelines used in the Arctic have unique challenges and stringent design conditions that must be met to ensure reliable operations in such remote and sensitive environments. To avoid flow assurance risks, the adage “the hotter the better” is in stark contrast to the sensitive nature of the Arctic environment to temperature changes, and where “the colder the better” is more appropriate. Permafrost, and its potential disturbance, is the most important factor to be considered for pipeline thermal design. High temperatures can disturb the in-situ state of the permafrost, causing settlement and instability in the permafrost zone. Also, high pipeline temperatures demand deep trenches to avoid melting the surface ice, challenging installation and increasing CAPEX. Designing the pipeline to maintain high internal fluid temperatures to reduce flow assurance risks and lower pipeline outer temperatures to minimize the impact on the environment is the best solution. To maintain high fluid temperatures and reduce heat loss to the environment, the conventional idea of a high value insulation like pipe-in-pipe with a vacuum annulus to avoid heat loss to the sensitive Arctic surroundings may seem to be a good solution, but it may not be the optimal solution. This paper discusses a hypothetical scenario (based on field cases) of a multiphase pipeline design and highlights the associated flow assurance/operational risks.


Author(s):  
A. P. Hoskins ◽  
R. A. Rankin ◽  
B. G. Motes ◽  
J. O. Carlson ◽  
C. W. Lagle ◽  
...  

2021 ◽  
pp. 14-38
Author(s):  
Klaus Dodds ◽  
Jamie Woodward

‘The physical environment’ describes the Arctic as the polar opposite of the Antarctic continent as it is an ocean semi-enclosed by land. The rocks of the Arctic record key periods in Earth history. The Arctic environment has had an interesting path of evolution. Why is the Arctic cold today? The polar latitudes actually receive less solar energy than the rest of the Earth's surface. What is the key role of sea ice in the Arctic climate system? How does sea ice decline impact upon the Arctic Ocean? The Greenland ice sheet, high latitude glaciers, and the importance of permafrost in the far north are also important topics related to the physical environment.


1938 ◽  
Vol 70 (7) ◽  
pp. 151-154 ◽  
Author(s):  
H. G. James

The following notes were made from a study of several species of Arctic Coollembola collected by Mr. W. J. Brown, of the Division of Entomology, Ottawa. Mr. Brown accompanied the voyage of the Canadian Arctic Patrol during August and September, 1935. During the trip he was able to collect on the southern shore of Baffin Island, and also well within the Arctic Circle as far north as Ellesmere Island.


2018 ◽  
Vol 38 (10) ◽  
pp. 769-772
Author(s):  
Yu. G. Kabaldin ◽  
D. A. Shatagin ◽  
A. V. Kiselev ◽  
M. V. Zhelonkin ◽  
A. A. Golovin
Keyword(s):  

2020 ◽  
Author(s):  
Valery Grebenets ◽  
Vasily Tolmanov ◽  
Vladimir Fedin ◽  
Anton Sinitskiy

<p>The department traditionally holds specialized practices of cryolithology and glaciology. Recently, specialized field course (sometimes international) have been concentrated in the Arctic region of Russia in the south of Yamal. The studies were focused on the investigation of the permafrost features in the regions, on assessing the permafrost dynamics and processes, affected by the various number of factors.</p><p>Here, the results of studies dedicated to the assessment of dangerous cryogenic processes impact on the infrastructure of the far north are widely introduced. Unique studies of the level of deformation of the infrastructure of the northern settlements are carried out during the establishment and development of an unfavorable geocryological situation.  Monitoring observations are carried out both in natural and in urbanized conditions,  allow us to compare the intensity of the processes, evaluate the contribution of technogenesis and climatic changes.</p><p>Based on the research results, students and researchers receive the necessary data and field results for analyzing the dynamics and changes in geotechnical systems in the context of an increase in the technogenic press and temperature increase in the region.</p><p>Investigation is supported by the <strong>RFBR project 18-05-60080</strong> “Dangerous nival-glacial and cryogenic processes and their influence on infrastructure in the Arctic”</p><p> </p>


2008 ◽  
Vol 27 (2) ◽  
pp. 164-187 ◽  
Author(s):  
Torben Wolff

The Danish Ingolf Expedition took place in the summer months of 1895 and 1896, with C. F. Wandel as captain, a man with long experience in hydrographical work in the Arctic. The other scientific participants were the zoologists H. Jungersen, W. Lundbeck and H. J. Hansen during the 1895 cruise; C. Wesenberg-Lund replaced Hansen during the 1896 cruise. C. H. Ostenfeld was the botanist and M. Knudsen the hydrographer. The Ingolf (see Figure 1) was a naval cruiser. In both years the voyages were hindered by ice that had moved much further south than normal, even closing most of the Denmark Strait. In 1895, the best results were obtained south of Iceland and in the Davis Strait; in 1896 south and east of Iceland and as far north as Jan Mayen Island. A total of 144 stations were completed, all with soundings, trawlings and (for the first time) continuous hydrographical work associated with the deep-sea trawling (bottom measurements of temperature, salinity, chlorine contents and specific gravity). Eighty of the stations were deeper than 1,000 m. There were more than 800 hydrographical measurements, with about 3,300 registrations recordings added on the basis of the measurements. 138 gas analyses were performed on board with samples from the surface and the sea bottom. The main result of the expedition was the final demonstration of probably the most important threshold boundaries in the world: the Wyville Thompson Ridge from East Greenland to Scotland with maximum depths of 600 m, separating the fauna in the Norwegian and Polar Sea to the north, always with negative below-zero temperatures except close to the Norwegian coast, from the fundamentally different general Atlantic deep-sea fauna to the south of the ridge with positive temperatures. The results are published in the Ingolf Report, with fifteen volumes containing forty-three papers by nineteen Danish authors and fourteen papers by six foreign authors. The sieving technique was excellent—due to an apparatus designed by H. J. Hansen that kept the animals under water until preservation and using the finest silk for sieving. In this way, the expedition collected more smaller animals than had been acquired by previous deep-sea expeditions. Hansen's studies of the peracarid crustaceans and parasitic copepods and Lundbeck's report on the sponges were particularly noteworthy. The 130 photographs taken on board and on land by the ship's doctor William Thulstrup represent a cultural/historical treasure.


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