Flow Test Results – “Unexpected Water” – where has it come from?
Cement bond history and Analysis of Balcombe 2 well
Angus have encountered unexpected high pressure water in a section of the horizontal well.
The water produced was not expected, the Company’s testing team believes a small high-pressure water zone was intersected in the horizontal section of the well which will require isolation in the future. Currently, the testing team believes the water production is not from the main Kimmeridge Reservoir itself but through fractured communication.
Where has the “unexpected water” come from? There are a number of possible causes, some of which are:
Geological faults. There are two main faults; one near the well head, and the other near the end of the horizontal bore. There may be other smaller faults interconnecting geological layers.
Balcombe 1 (1986) well is only metres away and cementation of this well may have decayed and failed after 32 years. Balcombe 1 well reports indicate that the drillers had a lot of problems with cementing a salt section within the Purbeck.
One very simple answer might be that a poor cement job on the Balcombe 2 well (2013) has created a conduit whereby water from the aquifer has travelled down the borehole to the horizontal well.
Evidence of poor quality cementing:
From a report commissioned by Cuadrilla by Weatherford “Interpretation of Cement Bond Logs”. The logging was completed on the 31st August 2013, the interpretation on 19th November 2013. The analyst was Maciey Pawlowski.
The first two columns below have been taken from their “Table 3 The Summary of results.”
The formation column has been added to show the geology the borehole is going through.
Interval (ft) | General Comment | Formation |
90 – 110 | No reliable interpretation of cement quality can be given over this section. | Wadhurst Clay to
153 ft |
110-151 | Poor to moderate casing to cement bond and cement to formation. | Ashdown Beds Aquifer |
151-168 | Moderate casing to cement to formation. | Ashdown Beds Aquifer |
168-210 | Moderate to poor casing to cement bond and cement to formation. | Ashdown Beds Aquifer |
210-429 | Moderate to poor casing to cement bond and cement to formation. | Ashdown Beds Aquifer |
429-600 | Moderate to poor casing to cement bond and cement to formation. | Ashdown Beds Aquifer |
600-708 | Poor casing to cement bond and cement to formation. | Ashdown Beds Aquifer |
708-927 | Moderate to good casing to cement bond and cement to formation. | Ashdown Beds Aquifer to 830 ft
Lulworth/Durlston to 1,550 ft |
927-1048 | Poor casing to cement bond and cement to formation | Lulworth/Durlston |
1048-1082 | Good to moderate casing to cement bond and cement to formation. | Lulworth/Durlston |
1082-1198 | Moderate to poor casing to cement bond and cement to formation. | Lulworth/Durlston |
1198-1312 | Moderate casing to cement bond and cement to formation. | Lulworth/Durlston |
1312-1550 | Not tested | Lulworth/Durlston |
1550-1831 | Not tested | Portland/Purbeck |
1831-2340 | Not tested | Kimmeridge Clay |
2340-2590 | Not tested | Kimmeridge Micrite
(where the horizontal bore has been drilled) |
Note that there appears to have been no cement logging for the sections below 1312 feet. Sadly this includes the important and difficult salt section in the Purbeck.
Angus responded to the following question from a FFBRA member which is also detailed on Angus’ website
What are the results of the Cement Bond Logs?
The Cement Bond logs confirm the Balcombe-2Z cement job was performed to a high standard, utilising the highest quality cement. Further, the logs conclusively confirm the strong integrity of the well and its complete zonal isolation. Industry experts refer to this well as having ‘no communication’. Everything enters and leaves the well at the surface borehole as commanded by operators.
The cement bond logs were also referred to in the recent Community Liaison Meeting. The discrepancies above clearly require further investigation and explanation from the Operator and Authorities.
In 2013 when the well was originally drilled, a green dye was seen in the neighbouring gill streams which was suspected to be Fluorescein – a tracer dye. We will be asking the authorities whether there is a connection.
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