简介:ThepolycrystallinephaseWO3/g-C3N4wassynthesizedunderstirringusingtungstenicacid(H2WO4)andgraphiticcarbonnitride(g-C3N4)asrawmaterials.ThecatalystwascharacterizedbyX-raydiffraction(XRD),scanningelectronmicroscopy(SEM),energydispersivespectroscopy(EDS),theFouriertransforminfraredspectroscopy(FT-IR),andtheBrunauer-Emmett-Telleranalysis(BET).ThepolycrystallinephaseWO3/g-C3N4wasdeterminedbyXRDtechnique.TheoxidativedesulfurizationprocesswasinvestigatedusingWO3/g-C3N4asthecatalyst,30%hydrogenperoxide(H202)astheoxidant,and1-butyl-3-methylimidazoliumtetrafluoroborate([bmim]BF4)ionicliquids(ILs)astheextractant.Theoperatingconditions,includingH2WO4amount,ILdose,H2O2volume,temperature,catalystdosage,andtypesofsulfurcompounds,weresystematicallyresearched.Thedesulfurizationratecouldreach98.46%forremovingdibenzothiophene(DBT)fromthemodeloilunderoptimalreactionconditions.Inaddition,thecatalyticactivitywasslightlydecreasedafterfiverecyclesofcatalysts.Thereactionkineticsanalysisshowsthattheoxidativedesulfurizationsystemwasinaccordwiththefirst-orderreactionkineticsequation.Themechanismofoxidativedesulfurizationwasproposed.
简介:储集层是控制油层分布的重要因素,储集层特征研究是进行油气勘探开发的重要环节。通过对南堡凹陷高尚堡油田GB区块沙三^3亚段Ⅴ油层组的储集层特征分析以及G32-19井岩心实验孔隙度与渗透率分析数据的剖析可以看出,沙三^3亚段Ⅴ油层组的储集层沉积成因类型为扇三角洲前缘亚相的砂坝与席状砂微相,以粉砂岩、细砂岩、中砂岩为主。碎屑分选、磨圆程度差,搬运距离短,岩石结构、成分成熟度低,呈现近物源、快速沉积的特点。此外,储集层物性研究不仅是孔隙度和渗透率等的单一因素分析,而是搬运沉积作用、沉积环境和成岩作用等一系列因素的综合评价。综合分析储集层物性影响因素认为,该储集层埋深大(〉4000m),泥质含量偏高,压实、胺结等成岩作用发育,是导致原生孔隙减少、物性变差的主要原因;但溶蚀作用又使粒间溶孔发育,是使该储集层物性相对变好的因素,导致孔隙类型以粒间溶孔为主。因此,对单一储集层,评价其物性的优劣,必须从地质构造、沉积相带、岩石类型、成岩阶段、黏土矿物的绝对含量和相对含量、长百和碳酸盐岩颗粒的溶蚀等多方面进行,才能得出正确的结论。