16/10-4
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General information
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Wellbore history
GeneralWell 16/10-4 was drilled on the Trond prospect located in the northeast part of PL 101, which is southeast of the existing Sleipner field. The prospect was a north-south elongated salt-induced structure with dip closure in all directions. The main purpose was to test the hydrocarbon potential within the upper Jurassic (Hugin) formation in the prospect and to obtain representative cores of that sand package.Operations and resultsThe jack up installation "Transocean Nordic" arrived on location on June 25 1998. Spud was significantly delayed due to insufficient leg penetration. Gravel boats had to be employed to dump gravel around the spud cans. This operation took 141 hours. With the gravel dumping completed, the weather became rough and the spud cans could not be lifted according to the plan. It took 162 hours before the weather was sufficiently calm to proceed with the pre-loading. Exploration well 16/10-4 was finally spudded on July 11 1998 and drilled to a total depth of 2580 m in Permian Zechstein anhydrites. The well was drilled with seawater and bentonite sweeps down to 380 m, with KCl / PAC mud from 380 m to 1230 m, and with KCl /PAC / glycol mud from 1230 m to TD.All the formations encountered from top Balder were found above prognosis due to anomalous velocities in the gas chimney drilled by this well. The reservoir target (Hugin Formation) was encountered at 2474 m. (80 m below prognosis). The petrophysical properties of the reservoir were found to be good. The only interval with some gas shows was the Rogaland Group (1792-1888 m) where the total gas was between 2.6 and 4.4 % Ci-nC4, but no reservoir was encountered at this level. No direct shows were observed in the Hugin Formation and the total gas was below 0.1%. From FMT measurements, log analysis and all the information collected during the drilling phase, the reservoir was found to be water bearing. However, onshore geochemical analysis by Eni central laboratories in Milan reported significant traces of migrated hydrocarbons in core samples from 2478 to 2496 m and high levels of phenols with possible traces of altered oil in the FMT water sample.One core was cut from 2477 to 2504 m in the soft, unconsolidated Hugin Formation (Previous wells in the area suffered no core recovery). The median porosity of the core was 25% and the median permeability was 260 m. Eight FMT pre tests and one segregated sample were taken from the Hugin reservoir. All pressure tests were good and gave a clear water gradient of 0,102 bar/m in the reservoir. The sample recovered was a mixture of mud filtrate and formation water.The 16/10-4 well was permanently abandoned on 10 August as a dry well.TestingNo drill stem test was performed. -
Cuttings at the Norwegian Offshore Directorate
Cuttings at the Norwegian Offshore Directorate Cuttings available for sampling?YESCuttings at the Norwegian Offshore Directorate Cutting sample, top depth [m]Cutting samples, bottom depth [m]210.002580.00 -
Cores at the Norwegian Offshore Directorate
Cores at the Norwegian Offshore Directorate Core sample numberCore sample - top depthCore sample - bottom depthCore sample depth - uom12477.02499.5[m ]Cores at the Norwegian Offshore Directorate Total core sample length [m]22.5Cores at the Norwegian Offshore Directorate Cores available for sampling?YES -
Palynological slides at the Norwegian Offshore Directorate
Palynological slides at the Norwegian Offshore Directorate Sample depthDepth unitSample typeLaboratory1050.0[m]DCRRI1100.0[m]DCRRI1150.0[m]DCRRI1200.0[m]DCRRI1250.0[m]DCRRI1300.0[m]DCRRI1350.0[m]DCRRI1400.0[m]DCRRI1450.0[m]DCRRI1500.0[m]DCRRI1550.0[m]DCRRI1600.0[m]DCRRI1650.0[m]DCRRI1700.0[m]DCRRI1750.0[m]DCRRI1760.0[m]DCRRI1770.0[m]DCRRI1780.0[m]DCRRI1790.0[m]DCRRI1800.0[m]DCRRI1810.0[m]DCRRI1820.0[m]DCRRI1830.0[m]DCRRI1840.0[m]DCRRI1850.0[m]DCRRI1860.0[m]DCRRI1870.0[m]DCRRI1880.0[m]DCRRI2420.0[m]DCRRI2430.0[m]DCRRI2440.0[m]DCRRI2450.0[m]DCRRI2460.0[m]DCRRI2470.0[m]DCRRI2477.5[m]CGEOLAB2490.0[m]DCRRI2490.8[m]CGEOLAB2498.0[m]CGEOLAB2500.0[m]DCRRI2510.0[m]DCRRI2520.0[m]DCRRI2530.0[m]DCRRI2550.0[m]DCRRI2560.0[m]DCRRI2570.0[m]DCRRI2580.0[m]DCRRI -
Lithostratigraphy
Lithostratigraphy Top depth [mMD RKB]Lithostrat. unit11696597110411792179218201830188218881888194021722398239824082449244924742474254725472550 -
Composite logs
Composite logs Document nameDocument formatDocument size [MB]pdf0.23 -
Geochemical information
Geochemical information Document nameDocument formatDocument size [MB]pdf1.14 -
Documents – reported by the production licence (period for duty of secrecy expired)
Documents – reported by the production licence (period for duty of secrecy expired) Document nameDocument formatDocument size [MB].pdf53.64 -
Logs
Logs Log typeLog top depth [m]Log bottom depth [m]FMT GR24812527HDIL MAC DSL SP GR21042585HDIP GR21042585LWD - DPR RAW GR3802580VSP00 -
Casing and leak–off tests
Casing and leak–off tests Casing typeCasing diam.
[inch]Casing depth
[m]Hole diam.
[inch]Hole depth
[m]LOT/FIT mud eqv.
[g/cm3]Formation test typeCONDUCTOR30195.036205.00.00LOTSURF.COND.20373.026380.01.42LOTINTERM.13 3/81219.017 1/21230.01.70LOTINTERM.9 5/82104.012 1/42110.01.75LOTOPEN HOLE2580.08 1/22580.00.00LOT -
Drilling mud
Drilling mud Depth MD [m]Mud weight [g/cm3]Visc. [mPa.s]Yield point [Pa]Mud typeDate measured891.0570.0SPUD MUD2250.007.0SPUD MUD3801.2032.0KCL / PAC6481.2124.0KCL / PAC11791.6143.0KCL / PAC12301.3621.0KCL / PAC15001.3935.0KCL / PAC18671.4642.0KCL -PAC21101.5033.0KCL / PAC24701.3531.0DUMMY25041.4635.0KCL / PAC25801.4536.0KCL / PAC -
Pressure plots
Pressure plots The pore pressure data is sourced from well logs if no other source is specified. In some wells where pore pressure logs do not exist, information from Drill stem tests and kicks have been used. The data has been reported to the NPD, and further processed and quality controlled by IHS Markit.Pressure plots Document nameDocument formatDocument size [MB]pdf0.22