METHOD OF PERMAFROST ROCK BEDDING DELIMITATION

FIELD: mining. ^ SUBSTANCE: invention refers to gas and oil industry and can be used, in particular, to select technology of well building and construction, as well as to monitor technical condition thereof inside permafrost rocks (PFR) and in permafrost zone. According to proposed method, a well is...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Hauptverfasser: POLOZKOV ALEKSANDR VLADIMIROVICH, SALIKHOV ZUL'FAR SALIKHOVICH, SUTYRIN ALEKSANDR VIKTOROVICH, ORLOV ALEKSANDR VIKTOROVICH, POTAPOV ALEKSANDR GRIGOR'EVICH, ZINCHENKO IGOR' ALEKSANDROVICH, GAFTUNJAK PETR IVANOVICH, FILIPPOV VIKTOR PAVLOVICH, POLOZKOV KIM ALEKSANDROVICH
Format: Patent
Sprache:eng ; rus
Schlagworte:
Online-Zugang:Volltext bestellen
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page
container_issue
container_start_page
container_title
container_volume
creator POLOZKOV ALEKSANDR VLADIMIROVICH
SALIKHOV ZUL'FAR SALIKHOVICH
SUTYRIN ALEKSANDR VIKTOROVICH
ORLOV ALEKSANDR VIKTOROVICH
POTAPOV ALEKSANDR GRIGOR'EVICH
ZINCHENKO IGOR' ALEKSANDROVICH
GAFTUNJAK PETR IVANOVICH
FILIPPOV VIKTOR PAVLOVICH
POLOZKOV KIM ALEKSANDROVICH
description FIELD: mining. ^ SUBSTANCE: invention refers to gas and oil industry and can be used, in particular, to select technology of well building and construction, as well as to monitor technical condition thereof inside permafrost rocks (PFR) and in permafrost zone. According to proposed method, a well is drilled, temperature is measured in depth of a well and then geothermic gradient is defined. On the basis of the results of these measurements, lower boundary depth of PFR ground bed is defined. For this purpose, before temperature in well depth is measured, a casing string (CS) is let down in a well along its sidewall and cemented. After cementing of CS is completed, measurements of temperature inside a well are carried out in the process of cement setting during thermal recovery. The results of temperature measurements are used to plot temperature curve of a well depending on the depth of a well. According to the depressed temperature level of the temperature curve, upper zone of PFR mass bedding inside it and lower zone under it are indicated. Lower zone is the zone of thawed, cooled and/or waterflooded rocks with higher temperature level when the average temperature gradient does not exceed 0.02-0.05°C/m. Between them, an intermediate transition "step" zone is indicated. This is a zone with rapid increase in temperature and high value of temperature gradient (G = 0.06-0.45°C/m and higher). According to the temperature curve and indicated connection point of the "step", which is an intermediate, high-gradient temperature zone with lower thawed, cooled and/or waterflooded zone, the depth of PFR mass bedding is defined. Inside PFR mass, separate local zones of thawed rocks with higher temperature level, frozen zones with depressed temperature level and intermediate high-gradient temperature zones lying between them are indicated simultaneously. According to junction points of intermediate zones and thawed zones, the boundaries between thawed and frozen zones located inside PFR mass are defined. In this case, temperature measurements inside a well are made using a highly sensitive thermometer with intervals of temperature measurement in depth of not more than 0.1-0.2 m. ^ EFFECT: more accurate definition of bottom depth of permafrost rock mass. ^ 2 cl, 2 dwg
format Patent
fullrecord <record><control><sourceid>epo_EVB</sourceid><recordid>TN_cdi_epo_espacenet_RU2329370C1</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>RU2329370C1</sourcerecordid><originalsourceid>FETCH-epo_espacenet_RU2329370C13</originalsourceid><addsrcrecordid>eNrjZNDzdQ3x8HdR8HdTCHAN8nV0C_IPDlEI8nf2VnBydXHx9HNXcHH18fT1DHEM8fT342FgTUvMKU7lhdLcDApuriHOHrqpBfnxqcUFicmpeakl8UGhRsZGlsbmBs6GxkQoAQCXmSVx</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>patent</recordtype></control><display><type>patent</type><title>METHOD OF PERMAFROST ROCK BEDDING DELIMITATION</title><source>esp@cenet</source><creator>POLOZKOV ALEKSANDR VLADIMIROVICH ; SALIKHOV ZUL'FAR SALIKHOVICH ; SUTYRIN ALEKSANDR VIKTOROVICH ; ORLOV ALEKSANDR VIKTOROVICH ; POTAPOV ALEKSANDR GRIGOR'EVICH ; ZINCHENKO IGOR' ALEKSANDROVICH ; GAFTUNJAK PETR IVANOVICH ; FILIPPOV VIKTOR PAVLOVICH ; POLOZKOV KIM ALEKSANDROVICH</creator><creatorcontrib>POLOZKOV ALEKSANDR VLADIMIROVICH ; SALIKHOV ZUL'FAR SALIKHOVICH ; SUTYRIN ALEKSANDR VIKTOROVICH ; ORLOV ALEKSANDR VIKTOROVICH ; POTAPOV ALEKSANDR GRIGOR'EVICH ; ZINCHENKO IGOR' ALEKSANDROVICH ; GAFTUNJAK PETR IVANOVICH ; FILIPPOV VIKTOR PAVLOVICH ; POLOZKOV KIM ALEKSANDROVICH</creatorcontrib><description>FIELD: mining. ^ SUBSTANCE: invention refers to gas and oil industry and can be used, in particular, to select technology of well building and construction, as well as to monitor technical condition thereof inside permafrost rocks (PFR) and in permafrost zone. According to proposed method, a well is drilled, temperature is measured in depth of a well and then geothermic gradient is defined. On the basis of the results of these measurements, lower boundary depth of PFR ground bed is defined. For this purpose, before temperature in well depth is measured, a casing string (CS) is let down in a well along its sidewall and cemented. After cementing of CS is completed, measurements of temperature inside a well are carried out in the process of cement setting during thermal recovery. The results of temperature measurements are used to plot temperature curve of a well depending on the depth of a well. According to the depressed temperature level of the temperature curve, upper zone of PFR mass bedding inside it and lower zone under it are indicated. Lower zone is the zone of thawed, cooled and/or waterflooded rocks with higher temperature level when the average temperature gradient does not exceed 0.02-0.05°C/m. Between them, an intermediate transition "step" zone is indicated. This is a zone with rapid increase in temperature and high value of temperature gradient (G = 0.06-0.45°C/m and higher). According to the temperature curve and indicated connection point of the "step", which is an intermediate, high-gradient temperature zone with lower thawed, cooled and/or waterflooded zone, the depth of PFR mass bedding is defined. Inside PFR mass, separate local zones of thawed rocks with higher temperature level, frozen zones with depressed temperature level and intermediate high-gradient temperature zones lying between them are indicated simultaneously. According to junction points of intermediate zones and thawed zones, the boundaries between thawed and frozen zones located inside PFR mass are defined. In this case, temperature measurements inside a well are made using a highly sensitive thermometer with intervals of temperature measurement in depth of not more than 0.1-0.2 m. ^ EFFECT: more accurate definition of bottom depth of permafrost rock mass. ^ 2 cl, 2 dwg</description><language>eng ; rus</language><subject>EARTH DRILLING ; EARTH DRILLING, e.g. DEEP DRILLING ; FIXED CONSTRUCTIONS ; MINING ; OBTAINING OIL, GAS, WATER, SOLUBLE OR MELTABLE MATERIALS OR ASLURRY OF MINERALS FROM WELLS</subject><creationdate>2008</creationdate><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://worldwide.espacenet.com/publicationDetails/biblio?FT=D&amp;date=20080720&amp;DB=EPODOC&amp;CC=RU&amp;NR=2329370C1$$EHTML$$P50$$Gepo$$Hfree_for_read</linktohtml><link.rule.ids>230,309,781,886,25568,76551</link.rule.ids><linktorsrc>$$Uhttps://worldwide.espacenet.com/publicationDetails/biblio?FT=D&amp;date=20080720&amp;DB=EPODOC&amp;CC=RU&amp;NR=2329370C1$$EView_record_in_European_Patent_Office$$FView_record_in_$$GEuropean_Patent_Office$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>POLOZKOV ALEKSANDR VLADIMIROVICH</creatorcontrib><creatorcontrib>SALIKHOV ZUL'FAR SALIKHOVICH</creatorcontrib><creatorcontrib>SUTYRIN ALEKSANDR VIKTOROVICH</creatorcontrib><creatorcontrib>ORLOV ALEKSANDR VIKTOROVICH</creatorcontrib><creatorcontrib>POTAPOV ALEKSANDR GRIGOR'EVICH</creatorcontrib><creatorcontrib>ZINCHENKO IGOR' ALEKSANDROVICH</creatorcontrib><creatorcontrib>GAFTUNJAK PETR IVANOVICH</creatorcontrib><creatorcontrib>FILIPPOV VIKTOR PAVLOVICH</creatorcontrib><creatorcontrib>POLOZKOV KIM ALEKSANDROVICH</creatorcontrib><title>METHOD OF PERMAFROST ROCK BEDDING DELIMITATION</title><description>FIELD: mining. ^ SUBSTANCE: invention refers to gas and oil industry and can be used, in particular, to select technology of well building and construction, as well as to monitor technical condition thereof inside permafrost rocks (PFR) and in permafrost zone. According to proposed method, a well is drilled, temperature is measured in depth of a well and then geothermic gradient is defined. On the basis of the results of these measurements, lower boundary depth of PFR ground bed is defined. For this purpose, before temperature in well depth is measured, a casing string (CS) is let down in a well along its sidewall and cemented. After cementing of CS is completed, measurements of temperature inside a well are carried out in the process of cement setting during thermal recovery. The results of temperature measurements are used to plot temperature curve of a well depending on the depth of a well. According to the depressed temperature level of the temperature curve, upper zone of PFR mass bedding inside it and lower zone under it are indicated. Lower zone is the zone of thawed, cooled and/or waterflooded rocks with higher temperature level when the average temperature gradient does not exceed 0.02-0.05°C/m. Between them, an intermediate transition "step" zone is indicated. This is a zone with rapid increase in temperature and high value of temperature gradient (G = 0.06-0.45°C/m and higher). According to the temperature curve and indicated connection point of the "step", which is an intermediate, high-gradient temperature zone with lower thawed, cooled and/or waterflooded zone, the depth of PFR mass bedding is defined. Inside PFR mass, separate local zones of thawed rocks with higher temperature level, frozen zones with depressed temperature level and intermediate high-gradient temperature zones lying between them are indicated simultaneously. According to junction points of intermediate zones and thawed zones, the boundaries between thawed and frozen zones located inside PFR mass are defined. In this case, temperature measurements inside a well are made using a highly sensitive thermometer with intervals of temperature measurement in depth of not more than 0.1-0.2 m. ^ EFFECT: more accurate definition of bottom depth of permafrost rock mass. ^ 2 cl, 2 dwg</description><subject>EARTH DRILLING</subject><subject>EARTH DRILLING, e.g. DEEP DRILLING</subject><subject>FIXED CONSTRUCTIONS</subject><subject>MINING</subject><subject>OBTAINING OIL, GAS, WATER, SOLUBLE OR MELTABLE MATERIALS OR ASLURRY OF MINERALS FROM WELLS</subject><fulltext>true</fulltext><rsrctype>patent</rsrctype><creationdate>2008</creationdate><recordtype>patent</recordtype><sourceid>EVB</sourceid><recordid>eNrjZNDzdQ3x8HdR8HdTCHAN8nV0C_IPDlEI8nf2VnBydXHx9HNXcHH18fT1DHEM8fT342FgTUvMKU7lhdLcDApuriHOHrqpBfnxqcUFicmpeakl8UGhRsZGlsbmBs6GxkQoAQCXmSVx</recordid><startdate>20080720</startdate><enddate>20080720</enddate><creator>POLOZKOV ALEKSANDR VLADIMIROVICH</creator><creator>SALIKHOV ZUL'FAR SALIKHOVICH</creator><creator>SUTYRIN ALEKSANDR VIKTOROVICH</creator><creator>ORLOV ALEKSANDR VIKTOROVICH</creator><creator>POTAPOV ALEKSANDR GRIGOR'EVICH</creator><creator>ZINCHENKO IGOR' ALEKSANDROVICH</creator><creator>GAFTUNJAK PETR IVANOVICH</creator><creator>FILIPPOV VIKTOR PAVLOVICH</creator><creator>POLOZKOV KIM ALEKSANDROVICH</creator><scope>EVB</scope></search><sort><creationdate>20080720</creationdate><title>METHOD OF PERMAFROST ROCK BEDDING DELIMITATION</title><author>POLOZKOV ALEKSANDR VLADIMIROVICH ; SALIKHOV ZUL'FAR SALIKHOVICH ; SUTYRIN ALEKSANDR VIKTOROVICH ; ORLOV ALEKSANDR VIKTOROVICH ; POTAPOV ALEKSANDR GRIGOR'EVICH ; ZINCHENKO IGOR' ALEKSANDROVICH ; GAFTUNJAK PETR IVANOVICH ; FILIPPOV VIKTOR PAVLOVICH ; POLOZKOV KIM ALEKSANDROVICH</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-epo_espacenet_RU2329370C13</frbrgroupid><rsrctype>patents</rsrctype><prefilter>patents</prefilter><language>eng ; rus</language><creationdate>2008</creationdate><topic>EARTH DRILLING</topic><topic>EARTH DRILLING, e.g. DEEP DRILLING</topic><topic>FIXED CONSTRUCTIONS</topic><topic>MINING</topic><topic>OBTAINING OIL, GAS, WATER, SOLUBLE OR MELTABLE MATERIALS OR ASLURRY OF MINERALS FROM WELLS</topic><toplevel>online_resources</toplevel><creatorcontrib>POLOZKOV ALEKSANDR VLADIMIROVICH</creatorcontrib><creatorcontrib>SALIKHOV ZUL'FAR SALIKHOVICH</creatorcontrib><creatorcontrib>SUTYRIN ALEKSANDR VIKTOROVICH</creatorcontrib><creatorcontrib>ORLOV ALEKSANDR VIKTOROVICH</creatorcontrib><creatorcontrib>POTAPOV ALEKSANDR GRIGOR'EVICH</creatorcontrib><creatorcontrib>ZINCHENKO IGOR' ALEKSANDROVICH</creatorcontrib><creatorcontrib>GAFTUNJAK PETR IVANOVICH</creatorcontrib><creatorcontrib>FILIPPOV VIKTOR PAVLOVICH</creatorcontrib><creatorcontrib>POLOZKOV KIM ALEKSANDROVICH</creatorcontrib><collection>esp@cenet</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>POLOZKOV ALEKSANDR VLADIMIROVICH</au><au>SALIKHOV ZUL'FAR SALIKHOVICH</au><au>SUTYRIN ALEKSANDR VIKTOROVICH</au><au>ORLOV ALEKSANDR VIKTOROVICH</au><au>POTAPOV ALEKSANDR GRIGOR'EVICH</au><au>ZINCHENKO IGOR' ALEKSANDROVICH</au><au>GAFTUNJAK PETR IVANOVICH</au><au>FILIPPOV VIKTOR PAVLOVICH</au><au>POLOZKOV KIM ALEKSANDROVICH</au><format>patent</format><genre>patent</genre><ristype>GEN</ristype><title>METHOD OF PERMAFROST ROCK BEDDING DELIMITATION</title><date>2008-07-20</date><risdate>2008</risdate><abstract>FIELD: mining. ^ SUBSTANCE: invention refers to gas and oil industry and can be used, in particular, to select technology of well building and construction, as well as to monitor technical condition thereof inside permafrost rocks (PFR) and in permafrost zone. According to proposed method, a well is drilled, temperature is measured in depth of a well and then geothermic gradient is defined. On the basis of the results of these measurements, lower boundary depth of PFR ground bed is defined. For this purpose, before temperature in well depth is measured, a casing string (CS) is let down in a well along its sidewall and cemented. After cementing of CS is completed, measurements of temperature inside a well are carried out in the process of cement setting during thermal recovery. The results of temperature measurements are used to plot temperature curve of a well depending on the depth of a well. According to the depressed temperature level of the temperature curve, upper zone of PFR mass bedding inside it and lower zone under it are indicated. Lower zone is the zone of thawed, cooled and/or waterflooded rocks with higher temperature level when the average temperature gradient does not exceed 0.02-0.05°C/m. Between them, an intermediate transition "step" zone is indicated. This is a zone with rapid increase in temperature and high value of temperature gradient (G = 0.06-0.45°C/m and higher). According to the temperature curve and indicated connection point of the "step", which is an intermediate, high-gradient temperature zone with lower thawed, cooled and/or waterflooded zone, the depth of PFR mass bedding is defined. Inside PFR mass, separate local zones of thawed rocks with higher temperature level, frozen zones with depressed temperature level and intermediate high-gradient temperature zones lying between them are indicated simultaneously. According to junction points of intermediate zones and thawed zones, the boundaries between thawed and frozen zones located inside PFR mass are defined. In this case, temperature measurements inside a well are made using a highly sensitive thermometer with intervals of temperature measurement in depth of not more than 0.1-0.2 m. ^ EFFECT: more accurate definition of bottom depth of permafrost rock mass. ^ 2 cl, 2 dwg</abstract><oa>free_for_read</oa></addata></record>
fulltext fulltext_linktorsrc
identifier
ispartof
issn
language eng ; rus
recordid cdi_epo_espacenet_RU2329370C1
source esp@cenet
subjects EARTH DRILLING
EARTH DRILLING, e.g. DEEP DRILLING
FIXED CONSTRUCTIONS
MINING
OBTAINING OIL, GAS, WATER, SOLUBLE OR MELTABLE MATERIALS OR ASLURRY OF MINERALS FROM WELLS
title METHOD OF PERMAFROST ROCK BEDDING DELIMITATION
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-16T23%3A01%3A20IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-epo_EVB&rft_val_fmt=info:ofi/fmt:kev:mtx:patent&rft.genre=patent&rft.au=POLOZKOV%20ALEKSANDR%20VLADIMIROVICH&rft.date=2008-07-20&rft_id=info:doi/&rft_dat=%3Cepo_EVB%3ERU2329370C1%3C/epo_EVB%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true