Off Setting Kill and Choke Lines Friction Losses, a New Method for Deep Water Well Control

2001 ◽  
Author(s):  
Thierry Botrel ◽  
Patrick Isambourg
Keyword(s):  
Deep Water ◽  
New Method ◽  
Well Control ◽  
Water Well

MABOPP - New Diagnostics and Procedures for Deep Water Well Control

1999 ◽  
Author(s):  
John P. James ◽  
Iain M. Rezmer-Cooper ◽  
Sverre Kr Sørskår
Keyword(s):  
Deep Water ◽  
Well Control ◽  
Water Well

A New Method to Predict and Assessment the Risk of Shallow Water Flow in Deep-Water Drilling

2019 ◽  
Author(s):  
Huanhuan Wang ◽  
Jin Yang ◽  
Jiayao Hong ◽  
Dongyufu Zhang ◽  
Lingyu Meng ◽  
...  
Keyword(s):  
Shallow Water ◽  
Water Flow ◽  
Deep Water ◽  
New Method ◽  
Shallow Water Flow

Field Experience to Assess Efficiency of Scale Dissolver Treatment in a SubSea Deep Water Well

2006 ◽  
Author(s):  
Jose Sergio Daher ◽  
J. A. T. Gomes ◽  
Francisca Ferreira Rosario ◽  
Maria Carmen Moreira Bezerra ◽  
Vera Cristina Amorim ◽  
...  
Keyword(s):  
Deep Water ◽  
Field Experience ◽  
Water Well

Reducing Deep-Water Well Delivery Times and Cost - A Look at the Bonga Wells Journey to Competitiveness

2017 ◽  
Author(s):  
Kingsley Okenyi ◽  
Abayomi Apena ◽  
Ejiro Emifoniye ◽  
Edgar Mba Ognane ◽  
Ejiro Ogbodu ◽  
...  
Keyword(s):  
Deep Water ◽  
Delivery Times ◽  
Water Well

Enhanced calving rates related to meltwater plume occurrence at Eqip Sermia, Greenland

2021 ◽  
Author(s):  
Adrien Wehrlé ◽  
Martin P Lüthi ◽  
Andrea Walter ◽  
Guillaume Jouvet ◽  
Andreas Vieli
Keyword(s):  
Deep Water ◽  
Quantitative Assessment ◽  
Power Index ◽  
Greenland Ice Sheet ◽  
Wave Activity ◽  
New Method ◽  
Wave Power ◽  
Dynamic Mass ◽  
Glacier Terminus ◽  
Minute Interval

<p>Glacier calving plays a key role in the recently observed dynamic mass<br>loss of the Greenland ice sheet. Calving waves, generated by the<br>sudden detachment of ice from the glacier terminus, can reach tens of<br>meters of height and have devastating effects upon impact on<br>surrounding shores. In this study, we describe a new method for the<br>detection of source location and timing of calving waves, and the<br>analysis of their magnitude and spreading properties using a<br>terrestrial radar interferometer (TRI). This method was applied to<br>11,500 minute-interval TRI acquisitions from Eqip Sermia, Greenland.<br>More than 2,000 calving waves were detected within seven<br>days. Quantitative assessment with a Wave Power Index (WPI) showed<br>spatially distinctive patterns: the sector of the calving front ending<br>in deep water shows a higher wave activity (+49%) with higher<br>cumulative WPI (+34%) than the shallow sector. In combination with<br>a detection of meltwater plume locations, we highlighted a 2.3 times<br>higher occurrence of visible meltwater plumes in the deep sector than the<br>shallow one. We found both the cumulated WPI and the number of waves<br>to increase by more than 80% in the presence of a meltwater plume<br>in the deep sector while only by 30% in the shallow sector.  We<br>therefore explain the higher calving activity in the deep sector to be <br>strongly related to a combination of higher occurrence of meltwater plumes <br>and more efficient calving enhancement linked to better connections <br>to deep warm waters.</p>

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