Assess the Impact of Shallow Water Flow Geohazard on Drilling Operations in the Riserless Sections of Deepwater Well Construction

Nitin R. Kulkarni, L. Heinze
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引用次数: 1

Abstract

Riserless drilling of the upper intervals of subsea wells has been standard practice in deepwater well construction, while taking mud returns to the sea floor. It has dramatically increased the safety of drilling shallow sections of subsea wells by reducing the hazard of handling gas at the rig, should shallow gas zones be encountered. It has also been very beneficial in controlling shallow water flows in deepwater areas of the Gulf of Mexico (GOM). The shallow water flow (SWF) is a typical offshore drilling hazard, defined as the phenomenon involving the flow of water from the surrounding region of a casing up to the ocean floor together with formation sands and sometimes free gas. The flowing water is driven by a pressure difference that occurs when the drill bit has encountered the unconsolidated but over-pressured sand sections. In the past 40 years of drilling practices, the SWF hazard has been experienced in several deep-water basins around the world, especially in the deep-water area where the water depth ranges from 1300 to 8200 ft and the formation depth ranges from 300 to 4000 ft below mud line (BML). Shallow water flows from overpressure aquifers have been a serious concern in the deepwater Gulf of Mexico for drilling and production operations. They can create significant financial and operational risks for exploration and development projects. In the GOM, SWF intervals typically occur between 300 and 2,500 ft BML and in water depths greater than 1,500 ft. If left unchecked, the disturbance from the water flow can cause loss of soil strength surrounding the wellbore, thereby compromising the structural integrity of the well. In extreme cases, SWFs have led to collapsed casing and/or total loss of wellbores. The paper aims to present the origin of shallow water flows in a deepwater environment and mitigation strategies adopted by industry to carry out the operations safely.
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评估浅水流动地质灾害对深水钻井施工无隔水管段钻井作业的影响
在深水钻井施工中,无隔水管钻井已成为标准做法,同时将泥浆带回海底。如果遇到浅层天然气区,它可以减少在钻井平台上处理天然气的危险,从而大大提高了钻井浅层海底井的安全性。它在控制墨西哥湾深水区浅水流动方面也非常有益。浅水流动(SWF)是一种典型的海上钻井危害,是指从套管周围区域流出的水与地层砂(有时还有游离气体)一起流向海底的现象。当钻头遇到未固结但压力过大的砂段时,就会产生压力差,从而驱动水流。在过去40年的钻井实践中,世界各地的几个深水盆地都经历过SWF危害,特别是在水深1300至8200英尺、地层深度300至4000英尺的深水区域。来自超压含水层的浅水流动一直是墨西哥湾深水钻井和生产作业的一个严重问题。它们会给勘探和开发项目带来巨大的财务和运营风险。在墨西哥湾,SWF层段通常位于300至2500英尺的水深,水深超过1500英尺。如果不加控制,水流的干扰会导致井筒周围土壤强度的损失,从而影响井的结构完整性。在极端情况下,主权财富基金会导致套管坍塌和/或井筒全部漏失。本文旨在介绍深水环境中浅水流的来源以及工业为安全开展作业而采取的缓解策略。
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