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《营救汪星人》西部“狗仔”海报曝光 国庆档唯一宠物合家欢类型电影_娱乐头条_大众网
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<meta name="Description" content='《营救汪星人》西部“狗仔”海报曝光。国庆档唯一宠物合家欢类型电影前方高能,一批头戴高顶毡帽、身背左轮手枪、脚穿高筒马靴的西部“狗仔”神气又炫酷的出场了。,《营救汪星人》西部“狗仔”海报曝光 国庆档唯一宠物合家欢类型电影' />
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  前方高能,一批头戴高顶毡帽、身背左轮手枪、脚穿高筒马靴的西部“狗仔”神气又炫酷的出场了。电影《营救汪星人》发布了西部“狗仔”造型写真,把“汪演员”的造型可塑性发挥到淋漓尽致,高顶毡帽、左轮手枪、高筒马靴一样不少,宣扬着“狗仔”精神,和向往自由、无比奔放的口号,可爱至极。据闻东部、南部、北部、中部的“狗仔”正列队向你跑来。   由星汇天姬出品的萌宠动作悬疑电影《营救汪星人》继上周发布了“戏精版金陵旗袍汪”、“太阳后裔军队汪”的主题海报后,这组由拉布拉多、英式博美、哈士奇、大头法斗、秋田、柯基、恶霸犬等十个品种狗狗演绎的“西部狗仔“主题海报又让观众眼前一亮。  《营救汪星人》由梁婷导演编剧,主演成毅、文松、阿拉蕾雅涵、唐本、林雪、欧弟、詹瑞文、王泷正、蓝博、赵宇彤等、以及周延GAI、郑则仕友情出演,联合30多个品种的200余只狗狗,开辟了华语电影大体量萌宠电影的先河,成为华语宠物电影狗出镜率最多的一部电影。此外,片中不仅集结了动作、飞车、公路、喜剧、强剧情的营救,在险象环生中与犯罪团伙斗智斗勇,让生命危在旦夕的汪星人重获自由。同时还释放能让“家长满意”的正能量主题,无疑满足了全年龄段观众们的胃口,是今年国庆档唯一宠物合家欢类型电影,影片将于日全国上映,据闻片方也于9月中下旬开启全国大规模的超前点映,敬请期待。
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致命守护者》新剧照曝光毒液“性感”身型。亦正亦邪善恶难辨由美国索尼哥伦比亚影业公司和漫威影业联合打造的电影《毒液:致命守护者》在近日频频放出重磅物料,既早前发布的“猛毒共生”版预告片后,今日又爆出以毒液全身为主体的新剧照。
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《盐酸盐溶液中温度对方解石和白云石溶解度的影响》
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大同建筑安装&#21457;&#31080;&#30005;&#9542;&#24494;&#92;&#20449;&#12304;&#49;&#53;&#56;&#49;&#42;&#51;&#51;&#49;&#48;&#42;&#57;&#55;&#49;&#12305;&#963;&#963;&#65307;&#12304;&#50;&#53;&#56;&#56;&#48;&#42;&#56;&#48;&#53;&#52;&#12305;&#32;&#21016;&#20250;&#35745;&#12290;&#12290;&#12290;&#12290;&#12290;&#12290;&#12290;&#38271;&#92;&#26399;&#92;&#26377;&#92;&#25928;&#9608;&#9608;&#9608;&#9608;&#9608;&#9608;&#9608;&#9608;&#27426;&#92;&#36814;&#92;&#21672;&#92;&#35810;&#46;&#20844;&#21496;&#32463;&#30334;&#24230;&#25512;&#24191;&#33;&#33;《盐酸盐溶液中温度对方解石和白云石溶解度的影响》
(盐)(酸)(盐)(溶)(液)(中)(温)(度)(对)(方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(的)(影)(响)(第)(22卷)(第)(4期)(2011年)(8月)(水)(资)(源)(与)(水)(工)(程)(JournalofWaterResourcesWaterEngineeringVo1.22NO.4Aug.,2011盐)(酸)(盐)(溶)(液)(中)(温)(度)(对)(方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(的)(影)(响)(梁)(冰)(,陈)(楠)(,姜)(利)(国)((辽)(宁)(工)(程)(技)(术)(大)(学)(力)(学)(与)(工)(程)(学)(院)(,辽)(宁)(阜)(新)(123000)摘)(要)(:为)(了)(更)(好)(的)(防)(止)(岩)(溶)(灾)(害)(的)(发)(生)(,研)(究)(了)(不)(同)(温)(度)(条)(件)(下)(盐)(酸)(盐)(溶)(液)(对)(石)(灰)(岩)(和)(白)(云)(岩)(侵)(蚀)(规)(律)(.应)(用)(美)(国)(地)(质)(调)(查)(所)(开)(发)(的)(水)(化)(学)(模)(拟)(软)(件)(Phreeqc对)(在)(不)(同)(CO:分)(压)(下)(,不)(同)(浓)(度)(的)(NaC1和)(MgC1溶)(液)(中)(的)(方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(和)(温)(度)(的)(关)(系)(进)(行)(了)(水)(化)(学)(模)(拟)(并)(进)(行)(了)(实)(验)(验)(证)(.研)(究)(结)(果)(显)(示)(,在)(NaC1溶)(液)(中)(,方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(均)(大)(于)(在)(纯)(水)(中)(的)(溶)(解)(度)(;方)(解)(石)(在)(MgC1溶)(液)(中)(的)(溶)(解)(度)(大)(于)(在)(同)(条)(件)(下)(NaC1溶)(液)(中)(的)(溶)(解)(度)(;无)(CO分)(压)(的)(情)(况)(下)(,在)(同)(浓)(度)(的)(盐)(溶)(液)(中)(,方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(迅)(速)(升)(高)(;在)(P…=10'MPa时)(,方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(而)(降)(低)(,然)(而)(始)(终)(大)(于)(在)(无)(CO:分)(压)(时)(的)(溶)(解)(度)(.在)(岩)(溶)(塌)(陷)(区)(,在)(与)(大)(气)(联)(系)(非)(常)(小)(的)(地)(下)(水)(系)(统)(中)(,温)(度)(的)(升)(高)(能)(够)(增)(强)(对)(岩)(体)(的)(侵)(蚀)(,从)(而)(使)(塌)(陷)(的)(危)(险)(增)(大)(;在)(与)(大)(气)(联)(系)(非)(常)(紧)(密)(的)(地)(下)(水)(系)(统)(中)(,温)(度)(降)(低)((大)(于)(0~C)能)(够)(增)(强)(对)(岩)(体)(的)(侵)(蚀)(,从)(而)(使)(塌)(陷)(的)(危)(险)(增)(大)(.关)(键)(词)(:Phreeqc软)(件)(;氯)(化)(物)(;方)(解)(石)(;白)(云)(石)(;溶)(解)(度)(;温)(度)(中)(图)(分)(类)(号)(:X43文)(献)(标)(识)(码)(:A文)(章)(编)(号)(:X(21.04Influenceoftemperatureondissolvingdegreesofcalciteanddolomiteinhvdr0chlOridesolutionLIANGBing.CHENNan,JIANGLiguo(SchoolofMechanicsandEngineering,LiaoningTechnicalUniversity,Fuxin123000,China)Abstract:Inordertopreventkarstdisaster,thepaperresearchedtheinfluenceofdissolvingdegreesoflimestoneanddolomitecausedbytemperatureinhydrochloridesolution.Awaterchemistrysimulationsoftware—pbreeqcdevelopedbyAmericanGeologicalInvestigationInstitutewasused,therelationmodelbetweentemperatureanddissolvingdegreesofcalciteanddolomitewassimulatedunderdifferentCO2pressureanddifferentconcentrationNaC1andMgC12solution,whichwastestedbyexperiment.TheresultsindicatedthatdissolvingdegreesofcalciteanddolomiteinNaC1solutionislargeThedissolvingdegreesofcalciteinMgC12solutionislargerthanthatinNaC1solutionundersamecondi—withoutCO2pressure,inthesameconcentrationsaltsolution,thedissolvingdegreesoflimestoneanddolomiteincreasedraWhilep..,:10一)(MPathereversehappened,butitislargerthanthatwithoutCO2pressure.Inkarstcollapsearea,theerosionofrockimprovedwithtempera—tureinereasement,whichcausedincreasementofthedangerdegreeofcollapseingroundwatersystemwhichhavenoobviousrelatiowhiletheerosionofrockincreasedwithreducingtemperature(1argerthan0?),SOastoenhuncethedangerdegreeofcollapseingroundwatersystem.Keywords:Ptemperature0引)(言)(随)(着)(经)(济)(的)(发)(展)(,由)(于)(地)(下)(水)(过)(度)(开)(采)(引)(发)(海)(水)(倒)(灌)(,工)(业)(污)(染)(物)(的)(大)(量)(排)(放)(,矿)(山)(开)(采)(等)(原)(因)(都)(能)(够)(引)(起)(地)(下)(水)(中)(氯)(化)(物)(浓)(度)(的)(升)(高)(….由)(于)(盐)(效)(应)(,方)(解)(石)(,白)(云)(石)(等)(矿)(物)(在)(不)(存)(在)(同)(离)(子)(效)(应)(的)(盐)(水)(中)(溶)(解)(度)(增)(大)(的)(现)(象)(前)(人)(早)(有)(认)(识)(.但)(是)(,除)(NaC1溶)(液)(可)(增)(大)(方)(解)(石)(的)(溶)(解)(度)(外)(,前)(人)(关)(于)(其)(他)(氯)(化)(物)(对)(方)(解)(石)(或)(白)(云)(石)(溶)(解)(度)(的)(影)(响)(很)(少)(进)(行)(研)(究)(.并)(且)(当)(盐)(效)(应)(和)(同)(离)(子)(效)(应)(同)(时)(存)(在)(时)(也)(多)(只)(是)(简)(单)(地)(认)(为)(盐)(效)(应)(可)(以)(忽)(略)(J.闫)(志)(为)(等)(认)(为)(溶)(液)(中)(的)(氯)(化)(物)(所)(产)(生)(的)(盐)(效)(应)(也)(将)(对)(碳)(酸)(盐)(的)(溶)(解)(产)(生)(很)(大)(的)(影)(响)(,他)(详)(细)(分)(析)(了)(25?时)(溶)(液)(中)(存)(在)(不)(同)(浓)(度)(氯)(化)(物)(对)(方)(解)(石)(和)(收)(稿)(日)(期)(:;修)(回)(日)(期)(:基)(金)(项)(目)(:国)(家)(自)(然)(科)(学)(基)(金)(资)(助)(项)(目)(();国)(家)(自)(然)(科)(学)(基)(金)(资)(助)(项)(目)(()的)(部)(分)(研)(究)(成)(果)(作)(者)(简)(介)(:梁)(冰)((1962.),女)(,辽)(宁)(盘)(锦)(人)(,教)(授)(,博)(士)(生)(导)(师)(,主)(要)(从)(事)(环)(境)(流)(体)(力)(学)(方)(面)(的)(研)(究)(工)(作)(.水)(资)(源)(与)(水)(工)(程)(20l1年)(白)(云)(石)(的)(溶)(解)(度)(的)(影)(响)(...考)(虑)(到)(由)(于)(南)(北)(方)(存)(在)(较)(大)(的)(温)(度)(差)(异)(,而)(且)(同)(一)(地)(区)(不)(同)(季)(节)(的)(温)(度)(差)(异)(也)(较)(大)(,所)(以)(有)(必)(要)(分)(析)(在)(复)(杂)(环)(境)(下)(温)(度)(对)(方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(的)(影)(响)(,从)(而)(推)(测)(出)(不)(同)(温)(度)(下)(氯)(化)(物)(溶)(液)(对)(石)(灰)(岩)(和)(白)(云)(岩)(产)(生)(的)(影)(响)(.本)(文)(运)(用)(水)(化)(学)(模)(拟)(方)(法)(就)(氯)(化)(物)(溶)(液)(中)(温)(度)(对)(方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(的)(影)(响)(进)(行)(模)(拟)(计)(算)(,分)(析)(温)(度)(对)(方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(的)(影)(响)(并)(为)(金)(属)(矿)(床)(岩)(溶)(现)(象)(提)(供)(更)(多)(水)(化)(学)(数)(据)(.Phreeqc是)(用)(C语)(言)(编)(写)(的)(在)(热)(力)(学)(原)(理)(和)(质)(量)(守)(恒)(理)(论)(的)(基)(础)(上)(建)(立)(的)(计)(算)(程)(序)(,可)(进)(行)(正)(向)(模)(拟)(与)(反)(向)(模)(拟)(,几)(乎)(能)(解)(决)(水)(,气)(,岩)(土)(相)(互)(作)(用)(系)(统)(中)(所)(有)(平)(衡)(热)(力)(学)(和)(化)(学)(动)(力)(学)(问)(题)(,包)(括)(水)(溶)(物)(配)(合)(,吸)(附)(一)(解)(析)(,离)(子)(交)(换)(,表)(面)(络)(合)(,溶)(解)(一)(沉)(淀)(,氧)(化)(还)(原)(.正)(向)(模)(拟)(能)(根)(据)(给)(定)(的)(反)(应)(机)(理)(来)(预)(测)(水)(的)(组)(分)(和)(质)(量)(的)(转)(移)(.主)(要)(运)(用)(反)(向)(模)(拟)(根)(据)(观)(测)(的)(化)(学)(和)(同)(位)(素)(资)(料)(来)(确)(定)(水)(岩)(反)(应)(机)(理)(,说)(明)(水)(流)(路)(径)(演)(化)(时)(所)(发)(生)(的)(化)(学)(变)(化)(,即)(计)(算)(造)(成)(水)(流)(路)(径)(上)(初)(始)(和)(最)(终)(水)(组)(分)(差)(异)(所)(必)(须)(溶)(解)(或)(析)(出)(的)(矿)(物)(和)(气)(体)(物)(质)(的)(量)(.1不)(同)(Pco2和)(温)(度)(条)(件)(下)(,在)(NaC1和)(MgC1:溶)(液)(中)(方)(解)(石)(,白)(云)(石)(溶)(解)(度)(的)(模)(拟)(模)(拟)(计)(算)(中)(选)(用)(不)(含)(CO:(P…=0MPa)和)(开)(放)(状)(态)(下)(存)(在)(大)(气)(c0分)(压)((P…=10MPa),温)(度)(为)(5,50?,NaC1和)(MgC1溶)(液)(的)(浓)(度)(为)(2000mmol/L和)(4000mmoL/L.计)(算)(中)(采)(用)(的)(平)(衡)(常)(数)(,焓)(,自)(由)(能)(等)(热)(力)(学)(常)(数)(取)(自)(Phreeqc软)(件)(所)(附)(带)(并)(得)(到)(学)(术)(界)(高)(度)(认)(可)(的)(Phreeqc.dat数)(据)(库)(.方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(分)(别)(采)(用)(其)(在)(不)(同)(条)(件)(下)(溶)(解)(平)(衡)((饱)(和)(指)(数)(SI=0)时)(的)(溶)(解)(量)(.模)(拟)(结)(果)(如)(图)(1,2,3,4所)(示)(.从)(模)(拟)(结)(果)(可)(看)(出)(方)(解)(石)(,白)(云)(石)(在)(不)(同)(温)(度)(和)(Pco2条)(件)(下)(,在)(NaC1和)(MgC1:溶)(液)(中)(的)(溶)(解)(度)(具)(有)(如)(下)(特)(征)(:(1)如)(图)(1所)(示)(,图)(中)(1和)(3为)(在)(无)(CO分)(压)(时)(,方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(;2和)(4为)(P=10-4.5MPa时)(,CO,分)(压)(时)(,方)(解)(石)(的)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(慢)(慢)(增)(大)(,白)(云)(石)(的)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(先)(有)(少)(量)(减)(小)(而)(后)(又)(增)(大)(.P…=10.MPa时)(,方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(不)(断)(减)(小)(.方)(解)(石)(在)(5~C时)(的)(溶)(解)(度)(为)(68.30mg/L,在)(50?时)(的)(溶)(解)(度)(为)(33.68mg/L,降)(低)(了)(2.03倍)(;白)(云)(石)(在)(5~C时)(的)(溶)(解)(度)(为)(87.51mg/L,在)(50~C时)(的)(溶)(解)(度)(为)(35.03mg/L,降)(低)(了)(2.5倍)(.?b.目)(黩)(建)(图)(1不)(同)(Pco2和)(温)(度)(条)(件)(下)(,方)(解)(石)(和)(自)(云)(石)(在)(纯)(水)(中)(的)(溶)(解)(度)(模)(拟)((2)图)(2中)(1,4为)(方)(解)(石)(和)(白)(云)(石)(在)(纯)(水)(中)(的)(溶)(解)(度)(;2,5为)(方)(解)(石)(和)(白)(云)(石)(在)(2000mmol/LNaC1溶)(液)(中)(的)(溶)(解)(度)(;3,6为)(方)(解)(石)(和)(白)(云)(石)(在)(4000mmo]/LNaC1溶)(液)(中)(的)(溶)(解)(度)(.可)(知)(,在)(无)(CO分)(压)(的)(条)(件)(下)(,在)(NaC1溶)(液)(中)(,方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(随)(温)(度)(的)(升)(高)(而)(上)(升)(的)(速)(率)(由)(快)(到)(慢)(为)(:2000mmol/LNaC1溶)(液)(4000mmol/LNaCl溶)(液)(纯)(水)(.图)(2无)(CO分)(压)(,不)(同)(温)(度)(条)(件)(下)(,方)(解)(石)(和)(白)(云)(石)(在)(NaC1溶)(液)(中)(的)(溶)(解)(度)(模)(拟)((3)图)(3中)(1,3为)(方)(解)(石)(在)(4000mmol/L的)(NaC1溶)(液)(中)(不)(同)(分)(压)(下)(的)(溶)(解)(度)(;2,4为)(方)(解)(石)(在)(2000mmol/L的)(MgC1,溶)(液)(中)(不)(同)(分)(压)(下)(的)(溶)(解)(度)(.可)(知)(,在)(同)(浓)(度)(cl一)(离)(子)(的)(溶)(液)(中)(,阳)(离)(子)(为)(Mg2离)(子)(的)(溶)(液)(中)(方)(解)(石)(的)(溶)(解)(度)(远)(大)(于)(阳)(离)(子)(为)(Na离)(子)(的)(溶)(液)(中)(方)(解)(石)(的)(溶)(解)(度)(.(4)由)(图)(4可)(知)(,在)(NaC1溶)(液)(中)(方)(解)(石)(的)(溶)(解)(度)(小)(于)(白)(云)(石)(的)(溶)(解)(度)(,而)(在)(MgC1溶)(液)(中)(方)(解)(石)(的)(溶)(解)(度)(远)(远)(大)(于)(白)(云)(石)(的)(溶)(解)(度)(.图)(4中)(:1.在)(无)(CO分)(压)(时)(,方)(解)(石)(在)(2000mmol/L的)(NaCI溶)(液)(中)(溶)(解)(度)(;2.在)(无)(CO分)(压)(时)(,方)(解)(石)(在)(2000mmol/L的)(MgC12溶)(液)(中)(溶)(解)(度)(;3.Pc0.=10-4.5MPa时)(,方)(解)(石)(在)(2000mmol/L的)(NaC1溶)(液)(中)(溶)(解)(度)(;4.Pc01=10MPa时)(,方)(解)(石)(在)(2000mmol/L第)(4期)(梁)(冰)(,等)(:盐)(酸)(盐)(溶)(液)(中)(温)(度)(对)(方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(的)(影)(响)(23的)(MgC1:溶)(液)(中)(溶)(解)(度)(;5.在)(无)(CO分)(压)(时)(,白)(云)(石)(在)(2000mmol/L的)(NaC1溶)(液)(中)(溶)(解)(度)(;6.在)(无)(CO分)(压)(时)(,白)(云)(石)(在)(2000mmol/L的)(MgC12溶)(液)(中)(溶)(解)(度)(;7.P=10-4.5MPa时)(,白)(云)(石)(在)(2000mmol/L的)(NaC1溶)(液)(中)(溶)(解)(度)(;8.P=10-4.5MPa时)(,白)(云)(石)(在)(2000mmol/L的)(MgC1溶)(液)(中)(溶)(解)(度)(.(5)由)(图)(4可)(知)(,在)(无)(CO分)(压)(的)(条)(件)(下)(,方)(解)(石)(和)(白)(云)(石)(在)(同)(浓)(度)(盐)(溶)(液)(中)(均)(随)(着)(温)(度)(的)(升)(高)(而)(升)(高)(;在)(时)(,方)(解)(石)(和)(白)(云)(石)(在)(同)(浓)(度)(盐)(溶)(液)(中)(均)(随)(着)(温)(度)(的)(升)(高)(而)(降)(低)(.然)(而)(,在)(时)(的)(溶)(解)(度)(却)(总)(大)(于)(在)(无)(CO分)(压)(的)(条)(件)(下)(的)(溶)(解)(度)(.例)(如)(,在)(无)(CO,分)(压)(的)(条)(件)(下)(,在)(2000mmol/L的)(NaC1溶)(液)(中)(,方)(解)(石)(在)(5?时)(的)(溶)(解)(度)(为)(54.14mg/L,在)(50~C时)(的)(溶)(解)(度)(为)(98.46mg/L,升)(高)(了)(1.82倍)(.在)(时)(,在)(2000mmol/L的)(NaC1溶)(液)(中)(,方)(解)(石)(在)(5?时)(的)(溶)(解)(度)(为)(156.96mg/L,在)(50qC时)(的)(溶)(解)(度)(为)(124.69mg/L,降)(低)(了)(20.4%.-??目)(V缝)(2实)(验)(原)(理)(与)(方)(法)((1)实)(验)(样)(品)(.方)(解)(石)(和)(白)(云)(石)(粉)(末)(,NaC1和)(MgC1,粉)(末)(,蒸)(馏)(水)(,电)(子)(秤)(.(2)实)(验)(原)(理)(与)(结)(果)(.实)(验)(装)(置)(如)(图)(5所)(示)(,检)(测)(在)(无)(CO影)(响)(时)(,不)(同)(浓)(度)(的)(NaC1和)(MgC1溶)(液)(对)(方)(解)(石)(和)(白)(石)(溶)(解)(度)(的)(影)(响)(.分)(别)(向)(容)(器)(中)(加)(入)(不)(同)(浓)(度)(的)(NaC1或)(MgC1溶)(液)(,用)(沸)(腾)(法)(排)(除)(溶)(液)(中)(的)(CO,再)(加)(人)(足)(量)(的)(方)(解)(石)(或)(白)(云)(石)(粉)(末)(,然)(后)(用)(密)(闭)(胶)(圈)(将)(装)(置)(封)(闭)(好)(,防)(止)(空)(气)(中)(的)(CO进)(入)(溶)(液)(中)(.然)(后)(放)(人)(到)(恒)(温)(箱)(中)(,通)(过)(水)(阀)(取)(得)(不)(同)(温)(度)(时)(的)(溶)(液)(,再)(用)(火)(焰)(原)(子)(吸)(收)(法)(测)(定)(溶)(液)(中)(含)(有)(的)(Ca的)(浓)(度)(,从)(而)(得)(到)(溶)(液)(中)(能)(够)(溶)(解)(的)(方)(解)(石)(或)(白)(云)(石)(的)(浓)(度)(.检)(测)(在)(开)(放)(状)(态)(下)(存)(在)(大)(气)(CO:分)(压)((P=10MPa)时)(,不)(同)(浓)(度)(的)(NaC1和)(MgC1,溶)(液)(对)(方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(的)(影)(响)(.方)(法)(与)(上)(同)(,不)(需)(要)(用)(沸)(腾)(法)(去)(除)(溶)(液)(中)(含)(有)(的)(CO.测)(定)(的)(结)(果)(见)(表)(1.胶)(圈)(/?温)(度)(/?温)(度)(图)(3不)(同)(温)(度)(条)(件)(下)(,方)(解)(石)(在)(NaC1图)(4不)(同)(Pco2和)(温)(度)(条)(件)(下)(,方)(解)(石)(和)(白)(云)(石)(图)(5溶)(解)(实)(验)(装)(置)(图)(和)(MgC1溶)(液)(中)(的)(溶)(解)(度)(模)(拟)(在)(NaC1和)(MgC1溶)(液)(中)(的)(溶)(解)(度)(模)(拟)(3模)(拟)(与)(实)(验)(结)(果)(分)(析)(对)(比)(实)(验)(测)(定)(结)(果)(与)(经)(Phreeqc软)(件)(计)(算)(得)(出)(的)(结)(果)(可)(知)(:在)(无)(CO分)(压)(时)(,模)(拟)(得)(出)(的)(结)(果)(要)(略)(小)(于)(实)(验)(得)(出)(的)(结)(果)(;而)(在)(开)(放)(状)(态)(下)(存)(在)(大)(气)(CO分)(压)((P…=10-4.5MPa)时)(,模)(拟)(得)(出)(的)(数)(据)(与)(实)(验)(得)(出)(数)(据)(相)(差)(很)(小)(.笔)(者)(分)(析)(是)(由)(于)(在)(排)(除)(溶)(液)(中)(的)(CO,时)(没)(有)(完)(全)(排)(除)(干)(净)(导)(致)(实)(验)(结)(果)(略)(有)(升)(高)(.所)(以)(,经)(Phreeqc软)(件)(的)(计)(算)(得)(出)(的)(结)(果)(是)(可)(靠)(的)(.结)(合)(现)(代)(水)(化)(学)(理)(论)(和)(前)(人)(的)(认)(识)(,对)(模)(拟)(与)(实)(验)(结)(果)(结)(果)(分)(析)(如)(下)(:(1)在)(P=10-4.5MPa时)(方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(而)(逐)(渐)(降)(低)(.产)(生)(这)(种)(现)(象)(的)(原)(因)(显)(然)(与)(溶)(解)(过)(程)(中)(CO,有)(关)(.闫)(志)(为)(认)(为)(这)(主)(要)(是)(由)(于)(CO溶)(于)(水)(形)(成)(HCO的)(反)(应)(受)(温)(度)(影)(响)(很)(大)(造)(成)(的)(.CO2(g)+H2O—H2CO3(aq)(1)按)(质)(量)(作)(用)(定)(律)(J,平)(衡)(时)(有)(:[H2CO3]…"?.'[H20][CO(g)]式)(中)(:K?为)(反)(应)(式)(的)(平)(衡)(常)(数)((无)(量)(纲)();方)(括)(号)(内)(各)(项)(为)(活)(度)(,mol/L,K随)(温)(度)(的)(增)(高)(明)(显)(降)(低)(圳)(.这)(也)(就)(是)(说)(,在)(相)(同)(P下)(,温)(度)(越)(高)(H,CO的)(活)(度)(越)(低)(.温)(度)(较)(高)(溶)(液)(中)(形)(成)(H也)(必)(然)(会)(少)(很)(多)(,因)(此)(该)(溶)(液)(对)(方)(解)(石)(,白)(云)(石)(的)(侵)(蚀)(性)(必)(然)(显)(着)(降)(低)(.(2)根)(据)(模)(拟)(结)(果)(认)(为)(,在)(NaC1溶)(液)(中)(,方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(均)(大)(于)(在)(纯)(水)(中)(的)(溶)(解)(度)(,是)(由)(于)(盐)(效)(应)(作)(用)(导)(致)(的)(.随)(着)(温)(度)(的)(升)(高)(,在)(不)(同)(浓)(度)(的)(NaC1溶)(液)(中)(,方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(的)(增)(大)(速)(率)(也)(不)(同)(,同)(温)(度)(下)(使)(方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(越)(高)(的)(NaC1溶)(液)(中)(,方)(解)(石)(和)(白)(云)(石)(随)(温)(度)(升)(高)(而)(增)(大)(水)(资)(源)(与)(水)(工)(程)(速)(率)(也)(越)(大)(,笔)(者)(分)(析)(是)(由)(于)(温)(度)(的)(升)(高)(能)(够)(增)(强)(盐)(效)(应)(的)(作)(用)(.(3)方)(解)(石)(在)(同)(浓)(度)(Cl一)(离)(子)(的)(溶)(液)(中)(,阳)(离)(子)(的)(溶)(液)(中)(方)(解)(石)(的)(溶)(解)(度)(远)(大)(于)(阳)(子)(为)(Mg离)(离)(子)(为)(Na离)(子)(的)(溶)(液)(中)(方)(解)(石)(的)(溶)(解)(度)(,是)(由)(于)(二)(价)(的)(Mg所)(形)(成)(溶)(液)(的)(离)(子)(强)(度)(要)(强)(于)(一)(价)(的)(Na,故)(MgC1溶)(液)(对)(石)(灰)(岩)(的)(侵)(蚀)(作)(用)(要)(比)(NaC1溶)(液)(的)(侵)(蚀)(作)(用)(要)(强)(很)(多)(.表)(1不)(同)(CO:与)(温)(度)(条)(件)(下)(,在)(NaC1和)(MgC12溶)(液)(中)(,方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(mg/L,?;mmol/L(4)白)(云)(石)(在)(MgC1溶)(液)(中)(的)(溶)(解)(度)(要)(比)(在)(NaC1溶)(液)(中)(小)(得)(多)(,主)(要)(是)(因)(为)(白)(云)(石)(溶)(解)(后)(能)(够)(溶)(解)(出)(Mg与)(MgC1:溶)(液)(中)(的)(Mg形)(成)(同)(离)(子)(效)(应)(,从)(而)(导)(致)(溶)(解)(度)(的)(降)(低)(.可)(以)(推)(测)(得)(出)(,CaC1溶)(液)(对)(石)(灰)(岩)(和)(白)(云)(岩)(的)(侵)(蚀)(作)(用)(都)(相)(对)(较)(小)(.(5)根)(据)(VantHoff方)(程)(式)(:i4oTlog(Kr)=log(Ko)+/'/丽)(r(3)式)(中)(:K,为)(给)(定)(温)(度)(()下)(的)(平)(衡)(常)(数)(;Ko为)(标)(准)(状)(态)(下)(的)(平)(衡)(常)(数)(;为)(热)(力)(学)(温)(度)(,;为)(热)(力)(学)(温)(度)((K),在)(此)(温)(度)(下)(测)(得)(的)(标)(准)(焓)(;R为)(通)(用)(气)(体)(常)(数)((8.315J/K?mo1)可)(知)(:随)(着)(温)(度)(的)(升)(高)(方)(解)(石)(溶)(解)(的)(平)(衡)(常)(数)(和)(白)(云)(石)(溶)(解)(的)(平)(衡)(常)(数)(都)(增)(大)(.Kc=『Ca]『CO,I3](4)Kd=[ca2][Mg][cO](5)式)(中)(方)(括)(弧)(内)(参)(量)(为)(各)(离)(子)(活)(度)(.由)(于)(溶)(液)(中)(各)(离)(子)(活)(度)(不)(变)(,为)(了)(使)(溶)(液)(中)(,增)(大)(,必)(将)(提)(高)(各)(离)(子)(的)(浓)(度)((活)(度)(=活)(度)(系)(数)(×浓)(度)(),从)(而)(提)(高)(矿)(物)(的)(溶)(解)(度)(,这)(就)(解)(释)(了)(盐)(效)(应)(随)(着)(温)(度)(的)(升)(高)(而)(增)(强)(的)(原)(因)(.无)(CO分)(压)(的)(情)(况)(下)(,在)(同)(浓)(度)(的)(盐)(溶)(液)(中)(,方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(迅)(速)(升)(高)(;在)(具)(有)(较)(大)(CO分)(压)(的)(情)(况)(下)(,方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(而)(降)(低)(,然)(而)(始)(终)(大)(于)(在)(无)(CO:分)(压)(时)(的)(溶)(解)(度)(.这)(就)(说)(明)(了)(CO在)(溶)(液)(中)(形)(成)(HCO所)(起)(的)(作)(用)(要)(强)(于)(盐)(效)(应)(对)(方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(的)(影)(响)(.据)(模)(拟)(结)(果)(可)(认)(为)(,在)(较)(低)(温)(度)(和)(较)(高)(P条)(件)(下)(的)(水)(中)(,方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(更)(大)(.4结)(语)(在)(无)(CO影)(响)(时)(,溶)(液)(内)(含)(有)(的)(Cl一)(离)(子)(浓)(度)(大)(小)(对)(石)(灰)(岩)(和)(白)(云)(岩)(侵)(蚀)(能)(力)(的)(影)(响)(,不)(随)(温)(度)(的)(改)(变)(而)(改)(变)(.能)(够)(产)(生)(越)(强)(盐)(效)(应)(的)(Cl一)(离)(子)(浓)(度)(下)(,方)(解)(石)(和)(白)(云)(石)(的)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(而)(增)(大)(的)(速)(率)(也)(越)(快)(;但)(在)(无)(cl一)(离)(子)(时)(,方)(解)(石)(和)(白)(云)(石)(溶)(解)(度)(随)(着)(温)(度)(的)(升)(高)(上)(升)(很)(少)(.笔)(者)(认)(为)(这)(时)(由)(于)(温)(度)(的)(升)(高)(可)(以)(增)(强)(盐)(效)(应)(的)(结)(果)(.可)(知)(在)(一)(些)(岩)(溶)(塌)(陷)(区)(,在)(与)(大)(气)(联)(系)(非)(常)(小)(的)(地)(下)(水)(系)(统)(中)(,温)(度)(的)(升)(高)(能)(够)(增)(强)(对)(岩)(体)(的)(侵)(蚀)(,从)(而)(使)(塌)(陷)(的)(危)(险)(增)(大)(.模)(拟)(结)(果)(显)(示)(当)(时)(,方)(解)(石)(和)(白)(云)(石)(在)(溶)(液)(中)((下)(转)(第)(3O页)()水)(资)(源)(与)(水)(工)(程)(2011年)(程)(1003m断)(面)(衬)(砌)(结)(构)(外)(侧)(,为)(0.17MPa.与)(单)(纯)(考)(虑)(水)(平)(地)(震)(荷)(载)(作)(用)(的)(情)(况)(相)(比)(较)(,在)(水)(平)(与)(竖)(向)(地)(震)(荷)(载)(的)(组)(合)(作)(用)(下)(,衬)(砌)(结)(构)(的)(应)(力)(分)(布)(规)(律)(基)(本)(相)(同)(,但)(应)(力)(值)(普)(遍)(增)(大)(,最)(大)(增)(幅)(可)(达)(单)(纯)(水)(平)(向)(地)(震)(荷)(载)(作)(用)(情)(况)(的)(21%.这)(说)(明)(在)(组)(合)(地)(震)(作)(用)(下)(,地)(下)(结)(构)(是)(偏)(于)(不)(安)(全)(的)(.因)(此)(,在)(进)(行)(调)(压)(井)(抗)(震)(设)(计)(时)(,为)(了)(准)(确)(而)(全)(面)(的)(掌)(握)(地)(下)(结)(构)(的)(地)(震)(反)(应)(,考)(虑)(水)(平)(和)(竖)(向)(地)(震)(的)(组)(合)(作)(用)(是)(必)(要)(的)(.5结)(语)(本)(文)(运)(用)(瞬)(态)(动)(力)(学)(方)(法)(,在)(进)(行)(调)(压)(井)(自)(振)(特)(性)(分)(析)(的)(基)(础)(上)(,按)(照)(单)(纯)(考)(虑)(水)(平)(地)(震)(荷)(载)(作)(用)(及)(考)(虑)(水)(平)(与)(竖)(向)(地)(震)(荷)(载)(组)(合)(作)(用)(两)(种)(计)(算)(工)(况)(,对)(不)(利)(围)(岩)(地)(质)(条)(件)(下)(施)(工)(期)(调)(压)(井)(的)(动)(力)(响)(应)(特)(性)(进)(行)(了)(有)(限)(元)(仿)(真)(分)(析)(.结)(果)(表)(明)(:(1)在)(单)(纯)(水)(平)(地)(震)(荷)(载)(作)(用)(下)(,地)(震)(荷)(载)(输)(入)(方)(向)(上)(衬)(砌)(结)(构)(的)(应)(力)(和)(位)(移)(时)(程)(变)(化)(幅)(度)(远)(大)(于)(其)(他)(方)(向)(,不)(同)(高)(程)(断)(面)(上)(应)(力)(和)(位)(移)(的)(时)(程)(变)(化)(趋)(势)(基)(本)(相)(同)(,同)(一)(断)(面)(上)(对)(称)(部)(位)(的)(应)(力)(和)(位)(移)(时)(程)(变)(化)(趋)(势)(相)(同)(,在)(调)(压)(井)(底)(部)(高)(程)(974m处)(存)(在)(一)(定)(的)(拉)(应)(力)(.(2)在)(水)(平)(与)(竖)(向)(地)(震)(荷)(载)(组)(合)(作)(用)(下)(,衬)(砌)(结)(构)(位)(移)(及)(应)(力)(的)(分)(布)(规)(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