RU2647545C1 - Method of determining ice boundary and ground while burning stamukh of hot water - Google Patents

Method of determining ice boundary and ground while burning stamukh of hot water Download PDF

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RU2647545C1
RU2647545C1 RU2017100875A RU2017100875A RU2647545C1 RU 2647545 C1 RU2647545 C1 RU 2647545C1 RU 2017100875 A RU2017100875 A RU 2017100875A RU 2017100875 A RU2017100875 A RU 2017100875A RU 2647545 C1 RU2647545 C1 RU 2647545C1
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ice
transparency
drilling
ground
depth
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RU2017100875A
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Russian (ru)
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Валентин Андреевич Морев
Виктор Витальевич Харитонов
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Федеральное государственное бюджетное учреждение "Арктический и Антарктический научно-исследовательский институт" (ФГБУ "ААНИИ")
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    • EFIXED CONSTRUCTIONS
    • E21EARTH OR ROCK DRILLING; MINING
    • E21CMINING OR QUARRYING
    • E21C39/00Devices for testing in situ the hardness or other properties of minerals, e.g. for giving information as to the selection of suitable mining tools

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  • Engineering & Computer Science (AREA)
  • Mining & Mineral Resources (AREA)
  • Life Sciences & Earth Sciences (AREA)
  • General Life Sciences & Earth Sciences (AREA)
  • Geochemistry & Mineralogy (AREA)
  • Geology (AREA)
  • Geophysics And Detection Of Objects (AREA)

Abstract

FIELD: ice-technology.
SUBSTANCE: invention relates to ice science and ice engineering and can be used in ice research, in particular in areas of hydrocarbon production on shelf of freezing seas. During process of thermal drilling of stamukha, speed of drilling and transparency of melt water near face are recorded on computer. As soon as thermobur passes through ice into ground, its transparency will decrease dramatically. In subsequent data processing on computer, dependence of drilling speed on depth and transparency of melt water is compared. Depth at which decrease in transparency of melt water occurred, corresponding to transition of drill from ice into ground, is defined as depth of ice and soil boundary.
EFFECT: technical result is to improve accuracy of determining boundary of ice and ground during drilling.
1 cl

Description

Изобретение относится к ледоведению и ледотехнике и может быть использовано в ледовых исследованиях, в частности, в районах добычи углеводородов на шельфе замерзающих морей.The invention relates to ice research and ice engineering and can be used in ice research, in particular in areas of hydrocarbon production on the shelf of freezing seas.

Стамуха представляет собой неподвижный торос, образовавшийся или придрейфовавший на мелководье и сидящий на грунте. Задачей исследования внутреннего строения льда является оценка возможных воздействий этих ледяных образований на различные морские сооружения.A ham is a stationary hummock, formed or drifted in shallow water and sitting on the ground. The task of studying the internal structure of ice is to assess the possible effects of these ice formations on various offshore structures.

Известные дистанционные методы исследования льда, такие как радиолокация и гидролокация, не могут обеспечить получение достоверных данных о внутреннем строении торосов и стамух из-за помех при зондировании неоднородного льда. Для таких исследований обычно проводят бурение скважин во льду с отбором или без отбора керна.Known remote ice research methods, such as radar and sonar, cannot provide reliable data on the internal structure of hummocks and hammers due to interference when probing heterogeneous ice. For such studies, drilling of wells in ice is usually carried out with or without coring.

Известен способ определения расположения границы льда и грунта при бурении стамух горячей водой [1, 2]. Во время бурения измеряют температуру талой воды вблизи забоя. Граница льда и грунта относительно поверхности льда расположена на глубине, при которой произошло резкое изменение температуры воды на забое и уменьшение скорости бурения до полной остановки термобура. Достоинством данного способа является достоверность определения расположения границы льда и грунта. Недостатком является неоднозначность при бурении стамухи остывшей рабочей водой из-за большого удаления водоподогревателя от объекта исследования или по иным причинам.There is a method of determining the location of the boundary of ice and soil when drilling stamukha hot water [1, 2]. During drilling, melt water temperature is measured near the bottom. The border of ice and soil relative to the ice surface is located at a depth at which a sharp change in the temperature of the water at the bottom and a decrease in the drilling speed until the thermal drill stops completely. The advantage of this method is the reliability of determining the location of the border of ice and soil. The disadvantage is the ambiguity when drilling the granite with cooled working water due to the large distance of the water heater from the object of study or for other reasons.

Целью настоящего изобретения является получение при водяном бурении объективной информации для определения расположения границы льда и грунта.The aim of the present invention is to obtain during water drilling objective information for determining the location of the boundary of ice and soil.

Указанная цель достигается следующими действиями:The specified goal is achieved by the following actions:

1. В процессе теплового бурения-плавления льда производят запись на компьютер скорости бурения и прозрачности талой воды. Как только термобур проходит сквозь лед в грунт, в скважине появляется взвесь воды и грунта или ила, и прозрачность ее резко уменьшится, даже если термобур продолжает погружаться, размывая грунт.1. In the process of thermal drilling-melting ice, the drilling speed and transparency of melt water are recorded on a computer. As soon as the thermal drill passes through the ice into the soil, a suspension of water and soil or silt appears in the well, and its transparency decreases sharply, even if the thermal drill continues to sink, eroding the soil.

2. При последующей обработке этих данных на компьютере сопоставляется зависимость скорости бурения с прозрачностью талой воды. Глубина, на которой произошло уменьшение прозрачности талой воды, соответствующее переходу бура изо льда в грунт, определяется как глубина расположения границы льда и грунта.2. During subsequent processing of these data on a computer, the dependence of the drilling speed on the transparency of melt water is compared. The depth at which there is a decrease in the transparency of melt water, corresponding to the transition of the drill from ice to soil, is defined as the depth of the location of the boundary between ice and soil.

Предлагаемый способ обеспечивает получение большого объема необходимой объективной информации о строении стамух. Экономический эффект от использования предлагаемого способа состоит из экономии времени высококвалифицированных специалистов при полевых работах. Учитывая повышенный интерес к строению торосистых образований в районах добычи углеводородов на шельфах замерзающих морей, настоящее предложение можно считать актуальным.The proposed method provides a large amount of necessary objective information about the structure of the gangs. The economic effect of using the proposed method consists in saving time of highly qualified specialists in the field. Given the increased interest in the structure of hummock formations in hydrocarbon production areas on the shelves of freezing seas, this proposal can be considered relevant.

Библиографические данныеBibliographic data

1. Морев В.А., Морев А.В., Харитонов В.В. Способ определения структуры торосов и стамух, свойств льда и границы льда и грунта. Патент на изобретение №2153070 от 20.07.2000. Бюллетень №20.1. Morev V.A., Morev A.V., Kharitonov V.V. A method for determining the structure of hummocks and hammers, the properties of ice and the boundary of ice and soil. Patent for invention No. 2153070 of 07.20.2000. Bulletin No. 20.

2. Victor V. Kharitonov and Valentin A. Morev. Computer recording of hot water drilling of ice ridges and stamukhas. Proc. of the 20th Int. Conference on Port and Ocean Engineering under Arctic Conditions (POAC). June 9-12, 2009,

Figure 00000001
, Sweden.2. Victor V. Kharitonov and Valentin A. Morev. Computer recording of hot water drilling of ice ridges and stamukhas. Proc. of the 20th Int. Conference on Port and Ocean Engineering under Arctic Conditions (POAC). June 9-12, 2009,
Figure 00000001
, Sweden.

Claims (1)

Способ определения расположения границы льда стамух и грунта, характеризующийся тем, что осуществляют тепловое водяное бурение скважин во льду с записью на компьютер или логгер скорости бурения и прозрачности талой воды вблизи забоя, при последующей обработке этих данных на компьютере сопоставляют зависимость скорости бурения с прозрачностью талой воды и глубину, на которой произошло уменьшение прозрачности талой воды, определяют как глубину расположения границы льда и грунта.A method for determining the location of the boundary between ice of Stamukha and soil, characterized in that thermal water drilling of wells in ice is carried out with the recording of the drilling speed and transparency of melt water near the bottom using a computer or logger, during subsequent processing of these data on a computer, the dependence of the drilling speed on the transparency of melt water is compared and the depth at which there has been a decrease in the transparency of melt water is defined as the depth of the location of the boundary between ice and soil.
RU2017100875A 2017-01-10 2017-01-10 Method of determining ice boundary and ground while burning stamukh of hot water RU2647545C1 (en)

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Citations (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
GB1575151A (en) * 1977-04-22 1980-09-17 Iceberg Transport Int Thermal drilling equipment
RU2153070C1 (en) * 1998-11-19 2000-07-20 Морев Валентин Андреевич Method of determining structure of ice hummocks and grounded ice hummocks, properties of ice and boundaries of ice and ground
RU2329370C1 (en) * 2006-11-07 2008-07-20 ООО "Ямбурггаздобыча" Method of permafrost rock bedding delimitation
RU2586348C2 (en) * 2012-01-19 2016-06-10 Халлибертон Энерджи Сервисез, Инк. Device for identifying minerals, as well as corresponding system and method

Patent Citations (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
GB1575151A (en) * 1977-04-22 1980-09-17 Iceberg Transport Int Thermal drilling equipment
RU2153070C1 (en) * 1998-11-19 2000-07-20 Морев Валентин Андреевич Method of determining structure of ice hummocks and grounded ice hummocks, properties of ice and boundaries of ice and ground
RU2329370C1 (en) * 2006-11-07 2008-07-20 ООО "Ямбурггаздобыча" Method of permafrost rock bedding delimitation
RU2586348C2 (en) * 2012-01-19 2016-06-10 Халлибертон Энерджи Сервисез, Инк. Device for identifying minerals, as well as corresponding system and method

Non-Patent Citations (3)

* Cited by examiner, † Cited by third party
Title
В.Н. СМИРНОВ и др., Исследования прочности, морфометрии и динамики льда в инженерных задачах при освоении шельфа в замерзающих морях, Проблемы арктики и антарктики, 2010, N 2. *
В.Н. СМИРНОВ и др., Исследования прочности, морфометрии и динамики льда в инженерных задачах при освоении шельфа в замерзающих морях, Проблемы арктики и антарктики, 2010, N 2. ХАРИТОНОВ В.В. и др., Метод исследования внутреннего строения торосов и стамух с помощью технологии термобурения, Метрология и гидрология, 2011, N 7, c. 49. *
ХАРИТОНОВ В.В. и др., Метод исследования внутреннего строения торосов и стамух с помощью технологии термобурения, Метрология и гидрология, 2011, N 7, c. 49. *

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