{"id":4787,"date":"2014-05-28T12:45:34","date_gmt":"2014-05-28T08:45:34","guid":{"rendered":"http:\/\/rion-journal.com\/?p=4787"},"modified":"2014-05-28T12:58:17","modified_gmt":"2014-05-28T08:58:17","slug":"5-2014","status":"publish","type":"post","link":"http:\/\/rion-journal.com\/en\/2014\/05\/28\/5-2014\/","title":{"rendered":"5-2014"},"content":{"rendered":"<p><a href=\"http:\/\/rion-journal.com\/wp-content\/uploads\/Nedra-05_14-1.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-4782\" alt=\"Nedra-05_14 .indd\" src=\"http:\/\/rion-journal.com\/wp-content\/uploads\/Nedra-05_14-1-212x300.jpg\" width=\"212\" height=\"300\" srcset=\"http:\/\/rion-journal.com\/wp-content\/uploads\/Nedra-05_14-1-212x300.jpg 212w, http:\/\/rion-journal.com\/wp-content\/uploads\/Nedra-05_14-1-106x150.jpg 106w, http:\/\/rion-journal.com\/wp-content\/uploads\/Nedra-05_14-1.jpg 724w, http:\/\/rion-journal.com\/wp-content\/uploads\/Nedra-05_14-1-400x566.jpg 400w\" sizes=\"auto, (max-width: 212px) 100vw, 212px\" \/><\/a><\/p>\n<table border=\"1\" cellspacing=\"0\" cellpadding=\"0\">\n<tbody>\n<tr>\n<td valign=\"top\" width=\"667\">\n<h3>CONTENTS<\/h3>\n<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 553.048:628.112:340.13<\/p>\n<p><b>Yazvin <\/b><b>A.<\/b><b>L. <\/b>(CJSC \u00abGYDEC\u00bb)<b> \/\/ <\/b><a href=\"mailto:alyazvin@hydec.ru\">alyazvin@hydec.ru<\/a><\/p>\n<p><b>A REVIEW OF REGULATORY AND LEGAL DOCUMENTS REGULATING THE EXPLORATION AND USE OF POTABLE AND INDUSTRIAL UNDERGROUND WATER SOURCES<\/b><\/p>\n<p>The regulatory and legal framework (as of 01.01.2014) regulating the exploration of underground water sources for potable and public water supply and process water supply to industrial facilities is reviewed in this article. The sequence of operations during geological explorations, construction and operation of water intake facilities is demonstrated. A comparison analysis of legislation norms on subsurface resources and related areas of law is carried out in this article.<\/p>\n<p><b>Key words: <\/b>legislation, regulatory and legal documents, potable and industrial underground water sources, subsurface management, licensing, reserve evaluation.<\/p>\n<p>\u0420. 3-10<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 556.3<\/p>\n<p><b>Borevskiy <\/b><b>B.<\/b><b>V.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:borevsky@hydec.ru\">borevsky@hydec.ru<\/a><\/p>\n<p><b>Markov M.L.<\/b> (FBGU \u00abGGI\u00bb) \/\/<b> <\/b><a href=\"mailto:2005mml@gmail.com\">2005mml@gmail.com<\/a><\/p>\n<p><b>IS RIVER LOW-WATER FLOW A MEASURE CONTRIBUTING TO UNDERGROUND WATER OR COMMON UNDERGROUND WATER INFLOW?<\/b><\/p>\n<p>An inflow correlation of underground waters and river low-water flow is considered in this article. It is demonstrated that this equalization is incorrect, since in most cases the low-water flow of rivers is less than ground water inflow. The article substantiates possible application of mean annual module for underground inflow into rivers instead of \u0420<sub>95%<\/sub> as it is practiced at present time in order to evaluate probable operational underground water reserves. A real example of ratio analysis of river flow rates and natural resources of underground water is considered in this article.<\/p>\n<p><b>Key words:<\/b> natural resources of underground water, operational underground water reserves, underground flow, underground inflow into rivers, underground water inflow, summer and winter low water periods.<\/p>\n<p>\u0420. 10-16<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 551. 345<\/p>\n<p><b>Abramov V.Yu.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:abramov@hydec.ru\">abramov@hydec.ru<\/a><\/p>\n<p><b>CRYOGENIC METAMORPHIZAITION CHEMICAL COMPOZITION OF UNDERGROUND WATER<\/b><\/p>\n<p>Underground water, ices, cryogenic salts, freezing and melt waters chemical composition cryogenic metamorphization is an inward change of concentration, composition at underground water cooling to zero and negative temperatures.<\/p>\n<p><b>Key words: <\/b>permafrost rock formations, freeze-out salt brines, cryogenic concentration, eutectics, eutectic salt content.<\/p>\n<p>\u0420. 16-20<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 556.3.06.532.5<\/p>\n<p><b>Ershov G.E.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/<b> <\/b><a href=\"mailto:ershov@hydec.ru\">ershov@hydec.ru<\/a><\/p>\n<p><b>ANALYSIS OF DATA ON ROUTINE OBSERVATIONS URGALSK COAL FIELD USING THE BALANCE MODEL<\/b><\/p>\n<p>The estimates of balance components of water inflow in underground workings Urgalsk field made using a mathematical model based on the balance of monitoring observations of precipitation, increase the area of mining and dewatering.<\/p>\n<p><b>Key words:<\/b> Urgalsk coal field, hydrogeological models, balance water influx, mine drainage, monitoring observations.<\/p>\n<p>\u0420. 20-26<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 550.83: 556.3<\/p>\n<p><b>Garaeva T.V.<\/b> (CJSC \u00abHYDEC\u00bb, the branch in the Republic of Tatarstan) \/\/ <a href=\"mailto:kazan@hydec.ru\">kazan@hydec.ru<\/a><\/p>\n<p><b>Gusakov I.O.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:info@hydec.ru\">info@hydec.ru<\/a><\/p>\n<p><b>Kozak S.Z. (<\/b>CJSC \u00abHYDEC\u00bb) \/\/<b> <\/b><a href=\"mailto:kozak@hydec.ru\">kozak@hydec.ru<\/a><\/p>\n<p><b>THE INTEGRATION OF GEOPHYSICAL METHODS IN IDENTIFYING PALEO-CHANNELS IN COMPLEX GEOLOGICAL AND HYDROGEOLOGICAL CONDITIONS BY THE EXAMPLE OF TATARSTAN<\/b><\/p>\n<p>The methodological application peculiarities of ground geophysics in complex geological and hydrogeological conditions are considered. A necessity to integrate electrical exploration and seismic exploration in identifying the land plots suitable for water boring operations in neogene deposits within Tatarstan is demonstrated.<\/p>\n<p><b>Key words:<\/b> underground water exploration, buried valley, integration of geophysical\u00a0methods, electrical prospecting, seismic prospecting.<\/p>\n<p>\u0420. 26-29<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 556.38: 556.182<\/p>\n<p><b>Borevskiy B.V.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:borevsky@hydec.ru\">borevsky@hydec.ru<\/a><\/p>\n<p><b>Yazvin A.L.<\/b> (CJSC \u00abHYDEC\u00bb)\/\/ <a href=\"mailto:alyazvin@hydec.ru\">alyazvin@hydec.ru<\/a><\/p>\n<p><b>Cherepanskiy M.M.<\/b> (MGRI-RGGRU) \/\/<b> <\/b><a href=\"https:\/\/e.mail.ru\/compose\/?mailto=mailto%3avodamch@mail.ru\">vodamch@mail.ru<\/a><\/p>\n<p><b>EXPERT EVALUATIONS OF UNDERGROUND WATER POTENTIAL RESERVE IN DEVELOPING COMPLEX USE AND WATER SUPPLY CONSERVATION SCHEMES<\/b><\/p>\n<p>The results of studies on regional evaluations of underground water potential reserves in the Russian Federation carried out at the turn of XX and XXI centuries by a department of the RF Ministry of Natural Resources under scientific-methodological supervision of GIDEK company are considered. A possible application of informational systems including factographic and cartographic databases for expert evaluations of possible intake volumes of underground water and its quality is demonstrated. The calculation principles for regional factors related to surface discharge reduction in connection with underground water intake are provided to substantiate joint use of underground and surface water sources.<\/p>\n<p><b>Key words: <\/b>underground water resource potential, complex use and water resources conservation schemes, industrial and potable water supply, informational systems.<\/p>\n<p>\u0420. 29-32<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 556.3: 553.048<\/p>\n<p><b>Borevskiy B.V.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:borevsky@hydec.ru\">borevsky@hydec.ru<\/a><\/p>\n<p><b>Yazvin A.L.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/<b> <\/b><a href=\"mailto:alyazvin@hydec.ru\">alyazvin@hydec.ru<\/a><\/p>\n<p><b>ONCE AGAIN ABOUT SIMPLIFIED REQUIREMENTS FOR EVALUATING UNDERGROUND WATER RESERVES FOR SMALL WATER INTAKES: PROBLEM STATUS AND POSSIBLE SOLUTIONS<\/b><\/p>\n<p>We have reviewed the issues related to evaluating underground water reserves within subsurface plots used by these water intake facilities. Legal regulation of subsurface management and negative consequences of existing work system, expert evaluation of their results, state record-keeping of water reserves. An analysis of possible criteria for differentiating subsurface plots is carried out. The term \u00abstandalone water intake facility\u00bb (\u00abstandalone water intake works\u00bb) is updated and the propositions to introduce simplified requirements for evaluating water reserves, contents and preparation of report materials are given.<b> <\/b><\/p>\n<p><b>Key words: <\/b>potable and industrial underground water, reserve evaluation, standalone water intake facility, law on \u00abSubsurface resources\u00bb, water ingress.<\/p>\n<p>\u0420. 32-39<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 504.062<\/p>\n<p><b>Nakhapetyan A.K.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:info@hydec.ru\">info@hydec.ru<\/a><\/p>\n<p><b>ABOUT HYDROGEOLOGICAL JUSTIFICATION OF UNDERGROUND WATER VULNERABILITY APPLIED TO CALCULATION OF SANITARY PROTECTION ZONES UNDERGROUND WATER INTAKE<\/b><\/p>\n<p>Examines a number of inconsistencies of SanPiN requirements to modern hydrogeological concepts about underground water vulnerability.<\/p>\n<p><b>Key words:<\/b> vulnerability, sanitary protection zones, underground water intake.<\/p>\n<p>\u0420. 39-40<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 556.3<\/p>\n<p><b>Garaeva T.V.<\/b> (CJSC \u00abHYDEC\u00bb, the branch in the Republic of Tatarstan) \/\/ <a href=\"mailto:kazan@hydec.ru\">kazan@hydec.ru<\/a><\/p>\n<p><b>NATURAL HYDROGEOLOGICAL MODEL FOR SVIYAZHSK UNDERGROUND WATER DEPOSIT IN THE REPUBLIC OF TATARSTAN<\/b><\/p>\n<p>This article reviews a natural hydrogeological model of Sviyazhsk potable underground water deposit \u2013 the only potable water supply source in Predvolzhie territory with limited water resources within the Republic of Tatarstan. The substantiation of this natural model is an essentially importance significance for target-oriented methodology of prospecting operations at Sviyazhsk deposit. The peculiarities of underground water formations determining their exploration and estimation procedure are reviewed in this article.<\/p>\n<p><b>Key words<\/b>: natural hydrogeological model, potable underground water, paleo-valley, sandy-argillaceous subsurface, underground water storage.<\/p>\n<p>\u0420. 40-44<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 553.98<\/p>\n<p><b>Abramov V.Yu. <\/b>(CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:abramov@hydec.ru\">abramov@hydec.ru<\/a><\/p>\n<p><b>FORMATION ORGANIC CARBON COMPOSITION OF COMPOUND CARBON DIOXIDE MINERAL WATERS OF THE ESSENTUKY, NAGUTSKY DEPOSITS<\/b><\/p>\n<p>The matters of the gas chemical consistent patterns of the formation of the composition of compound carbon dioxide mineral waters of the Essentuky and Nagutsky basin have been considered. A source of the formation of the carbon dioxide layout of mineral waters is thermal metamorphic supercritical fluids of \u041d<sub>2<\/sub>\u041e, \u0421\u041e<sub>2 <\/sub>\u0438 H<sub>2<\/sub>S (sc-fluid) entering from the crystalline basement and biogenic carbonic acid formed as a result of the biodegradation of light hydrocarbons of the petroleum series (\u0421 \u226410) migrating in the form extracted with CO<sub>2<\/sub> sc-fluids. When CO<sub>2<\/sub> sc-fluids are degradated to gas, hydrocarbons discharge in the form of an independent phase.<\/p>\n<p><b>Key words:<\/b> carbon dioxide mineral waters, supercritical fluids of CO<sub>2,<\/sub> H<sub>2<\/sub>S and H<sub>2<\/sub>O, extracted with CO<sub>2<\/sub> sc-fluids petroleum series, organic carbon composition.<\/p>\n<p>\u0420. 47-51<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 556.3<\/p>\n<p><b>Borevskiy B.V.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:borevsky@hydec.ru\">borevsky@hydec.ru<\/a><\/p>\n<p><b>Kozak<\/b><b> N.S.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:info@hydec.ru\">info@hydec.ru<\/a><\/p>\n<p><b>THE TYPE DESIGN OF COMBINED WATER INTAKE SYSTEMS IN JOINT USE OF UNDERGROUND AND SURFACE WATERS<\/b><\/p>\n<p>A new type design practice for combined water intake systems when underground and surface water sources are jointly used both in compensating mode and permanent operation mode of both water sources is offered in this article. The most efficient variants for compensating use of underground water sources with insufficient surface water sources are identified without any damage to the latter.<\/p>\n<p><b>Key words:<\/b> underground water sources, surface water sources, combined facilities, compensating water intake facility, catch basin.<\/p>\n<p>\u0420. 51-55<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 550.83: 556.3:551.34<\/p>\n<p><b>Kozak S.Z.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:kozak@hydec.ru\">kozak@hydec.ru<\/a><\/p>\n<p><b>THE IDENTIFICATION OF SUBGELISOL DURING WATER EXPLORATION USING GEOPHYSICAL METHODS<\/b><\/p>\n<p>The application features of geophysical methods in identifying subgelisol in solid and unconsolidated rocks are analyzed. The application practicability of water geophysics at the initial stage of studies with identification of underflow (underlake subgelisols) with further tracing of them as interpermafrost and subpermafrost subgelisols right on a work site.<\/p>\n<p><b>Key words:<\/b> subgelisols, ground and water geophysics, integration.<\/p>\n<p>\u0420. 55-57<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 556.3<\/p>\n<p><b>Palkin S.S.<\/b> (CJSC \u00abHYDEC\u00bb, Ural branch) \/\/ <a href=\"mailto:ural@hydec.ru\">ural@hydec.ru<\/a><\/p>\n<p><b>Kozak S.Z. <\/b>(CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:Kozak60@yandex.ru\">kozak@hydec.ru<\/a><\/p>\n<p><b>Ageev V.V.<\/b> (Geomagnetic research center under the Institute of Geophysics, RAS) \/\/ <a href=\"mailto:emrcinga@mtu-net.ru\">emrcinga@mtu-net.ru<\/a><\/p>\n<p><b>Kalneus E.V.<\/b> (Institute of Chemical Kinetics and Burning, RAS SB) \/\/ <a href=\"mailto:kalneus@kinetics.nsc.ru\">kalneus@kinetics.nsc.ru<\/a><\/p>\n<p><b>SUBGELISOL IDENTIFICATION EXPERIENCE IN A PERMAFROST ZONE OF YAMAL PENINSULA <\/b><\/p>\n<p>In connection with further intensive development of Yamal peninsula it is necessary to solve the problems with stable water supply to existing inhabited localities and to those planned to be constructed, hydrocarbon minding and processing facilities and their infrastructure. Until recently this possibility to use underground water sources for these purposes was estimated as of little promise due to historical perceptions that these resources are limited. A hydrogeological exploration experience obtained on Yamal over recent years makes it possible to change these perceptions and consider underground water sources as the most favorable source for potable water supply.<\/p>\n<p><b>Key words:<\/b> Yamal peninsula, permafrost formations, subgelisol water-bearing zone, fresh underground water sources.<\/p>\n<p>\u0420. 58-61<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 556.3.06.532.5<\/p>\n<p><b>Ershov G.E.<\/b> (CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:ershov@hydec.ru\">ershov@hydec.ru<\/a><\/p>\n<p><b>THE ANALYSIS OF CONDITIONS FOR FORMATION AND OPERATION OF FRESH UNDERGROUND WATER OF THE TROITSK FIELD OF ELISTA<\/b><\/p>\n<p>There is considered the schematization of hydrogeological conditions, the balance of freshwater lens formation Troitskoe field (Kalmykia) and its changes during the operation with the help of numerical hydrogeological model of the field. Limit values of water intake, in which there is no depletion of fresh water defined.<\/p>\n<p><b>Key words:<\/b> lenses of fresh water, numerical modeling, migration models, Kalmykia.<\/p>\n<p>\u0420. 61-66<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 550.8.013<\/p>\n<p><b>Zubanova T.N.<\/b> (CJSC \u00abHYDEC\u00bb, Lower Volga branch) \/\/ <a href=\"mailto:saratov@hydec.ru\">saratov@hydec.ru<\/a><\/p>\n<p><b>Shuvatkin K.N.<\/b> (CJSC \u00abHYDEC\u00bb, Lower Volga branch) \/\/ <a href=\"mailto:saratov@hydec.ru\">saratov@hydec.ru<\/a><\/p>\n<p><b>THE SUBSTANTIATION OF A GEOLOGICAL MODEL IN COMPLEX HYDROGEOCHEMICAL CONDITIONS BY THE EXAMPLE OF ZAPODNOBELOZERSK SUBSURFACE PLOT IN THE SOK RIVER VALLEY OF SAMARA REGION<\/b><\/p>\n<p>Reviews the formation peculiarities of underground water chemical compound in quaternary alluvial deposits within the Sok river valley. A hydrogeological model of Zapadnobelozersk subsurface plot is substantiated, the schematization data on filtration medium and hydrogeochemical parameters are provided, an optimal design option for water intake facilities in complex hydrogeochemical conditions is offered.<\/p>\n<p><b>Key words:<\/b> water supply, schematization, geologic filtration model, geologic migration model, model balance.<\/p>\n<p>\u0420. 66-69<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 550.8.013<\/p>\n<p><b>Pashnin A.Yu. <\/b>(CJSC \u00abHYDEC\u00bb, Lower Volga branch) \/\/ <a href=\"mailto:saratov@hydec.ru\">saratov@hydec.ru<\/a><\/p>\n<p><b>THE DEVELOPMENT PECULIARITIES OF A HYDRODYNAMIC MODEL FOR WASTE WATER PUMPING FIELD AT URITSKY HYDROCARBON DEPOSIT<\/b><\/p>\n<p>The main peculiarities of hydrogeological formation within Uritsky hydrocarbon deposit are characterized. A geologic filtration model of Uritsky discharge field is justified in the article, the filtration medium schematization and hydrogeochemical parameters data are provided in this article. The article describes the results of forecast task solutions and provides the efficient schemes for further operation of the field.<\/p>\n<p><b>Key words:<\/b> discharge field, field wastewater, geological filtration model, absorbing well, operation options.<\/p>\n<p>\u0420. 69-72<\/td>\n<\/tr>\n<tr>\n<td valign=\"top\" width=\"667\">\n<p align=\"right\">\u0423\u0414\u041a 556.182:556.332.6<\/p>\n<p><b>Belyakov M.V. <\/b>(CJSC \u00abHYDEC\u00bb) \/\/ <a href=\"mailto:mb@hydec.ru\">mb@hydec.ru<\/a><\/p>\n<p><b>THE RESULTS OF THE GROUP TEST-OPERATIONAL PUMPING AT ANOMALY HIGH FILTRATION ROCK PROPERTIES AT UDOMELSKY UNDERGROUND WATER DEPOSIT<\/b><\/p>\n<p>Maintenance of strict temperature mode of reactor blocks of atomic power plants is carried out by exploiting of natural or artificial reservoirs-coolers. Kalinin NPP is located at the watershed, so the surface water resources for cooling during warm seasons are not enough &#8211; there is a drastic decrease in the volume of water due to high evaporation and exceedances of water temperature in cooling ponds. One of the ways to resupply cooling lakes with a deficit of surface water resources is an attraction of low-temperature underground water.<\/p>\n<p><b>Key words<\/b>: Kalinin Nuclear Power Plant (KNPP), replenishment of cooling lakes, massive group test-operational pumping.<\/p>\n<p>\u0420. 72-76<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>\u00a0<\/p>\n<p>\u00a0<\/p>","protected":false},"excerpt":{"rendered":"<p>CONTENTS \u0423\u0414\u041a 553.048:628.112:340.13 Yazvin A.L. (CJSC \u00abGYDEC\u00bb) \/\/ alyazvin@hydec.ru A REVIEW OF REGULATORY AND LEGAL DOCUMENTS REGULATING THE EXPLORATION AND USE OF POTABLE AND INDUSTRIAL UNDERGROUND WATER SOURCES The regulatory and legal framework (as of 01.01.2014) regulating the exploration of underground water sources for potable and public water supply and process water supply to industrial [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":4782,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[20],"tags":[],"class_list":["post-4787","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-20"],"acf":[],"_links":{"self":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/posts\/4787","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/comments?post=4787"}],"version-history":[{"count":0,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/posts\/4787\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/media\/4782"}],"wp:attachment":[{"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/media?parent=4787"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/categories?post=4787"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/rion-journal.com\/en\/wp-json\/wp\/v2\/tags?post=4787"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}