This study analyzes the impact of circulation types(CTs)on ozone(O_(3))pollution in Beijing.The easterly high-pressure(SWW)circulation occurred most frequently(30%;276 day),followed by northwesterly high-pressure(AN)c...This study analyzes the impact of circulation types(CTs)on ozone(O_(3))pollution in Beijing.The easterly high-pressure(SWW)circulation occurred most frequently(30%;276 day),followed by northwesterly high-pressure(AN)circulation(24.3%;224 day).The SWW type had the highest O_(3) anomaly of+17.28μg/m^(3),which was caused by excellent photochemical reactions,poor diffusion ability and regional transport.Due to the higher humidity and precipitation in the low-pressure type(C),the O_(3) increase(+8.02μg/m^(3))was less than that in the SWW type.Good diffusion/wet deposition and weak formation ability contributed to O_(3) decrease in AN(-12.54μg/m^(3))and northerly high-pressure(ESN)CTs(-12.26μg/m^(3)).The intra-area transport of O_(3) was significant in polluted circulations(SWW-and C-CTs).In addition,higher temperature,radiation and less rainfall also contributed to higher O_(3) in northern Beijing under the SWW type.For the clean CTs(AN and ESN CTs),precursor amount and intra-area transport played a dominant role in O_(3) distribution.Under the northeasterly low-pressure CT,better formation conditions and higher precursor amount combined with the intra-area southerly transport to cause higher O_(3) values in the south than in the north.The higher O_(3) in the northwestern area under the northeasterly high-pressure type was influenced by weaker titration loss and high O_(3) concentration in previous day.Annual variation in the CTs contributed up to 86.1%of the annual variation in O_(3).About 78%-83%of the diurnal variation in O_(3) resulted from local meteorological factors.展开更多
西藏尼木地区分布一套增生杂岩,其对冈底斯火山岩浆弧的演化具有重要意义。本文对该套增生杂岩中的变质火山岩的地质特征、矿物学、全岩地球化学和锆石U-Pb年代学等方面进行了综合研究。变质火山岩以斜长角闪岩、角闪斜长片麻岩为主,其...西藏尼木地区分布一套增生杂岩,其对冈底斯火山岩浆弧的演化具有重要意义。本文对该套增生杂岩中的变质火山岩的地质特征、矿物学、全岩地球化学和锆石U-Pb年代学等方面进行了综合研究。变质火山岩以斜长角闪岩、角闪斜长片麻岩为主,其中,角闪石主要为镁质角闪石,共生的斜长石主要为拉长石;变质火山岩经历了高温-中压变质作用;岩石富Al 2 O 3和贫TiO 2,弱富集轻稀土元素(LREE),富集Rb、Sr、Ba等大离子亲石元素(LILE),亏损Nb、Ta、Ti等高场强元素(HFSE),其地球化学特征与火山弧玄武岩的地球化学特征相似,其形成的构造环境为洋内岛弧或活动大陆边缘弧;岩浆锆石U-Pb年龄值为151.4±1.6Ma和150.7±1.4Ma,表明岩石的形成时代为晚侏罗世。综合研究认为,增生杂岩中的变质火山岩是新特提斯洋在晚侏罗世北向俯冲的产物,在陆-陆碰撞之前卷入增生系统,该套变质火山岩不是以往所认为的变质结晶基底。展开更多
基金supported by the Beijing Municipal Natural Science Foundation(No.8204075)the National Key Research and Development Program of China(No.2016YFC0203302)+2 种基金the National Natural Science Foundation of China(Nos.4147513591744206)the Beijing Nova Program(No.xx2017079).
文摘This study analyzes the impact of circulation types(CTs)on ozone(O_(3))pollution in Beijing.The easterly high-pressure(SWW)circulation occurred most frequently(30%;276 day),followed by northwesterly high-pressure(AN)circulation(24.3%;224 day).The SWW type had the highest O_(3) anomaly of+17.28μg/m^(3),which was caused by excellent photochemical reactions,poor diffusion ability and regional transport.Due to the higher humidity and precipitation in the low-pressure type(C),the O_(3) increase(+8.02μg/m^(3))was less than that in the SWW type.Good diffusion/wet deposition and weak formation ability contributed to O_(3) decrease in AN(-12.54μg/m^(3))and northerly high-pressure(ESN)CTs(-12.26μg/m^(3)).The intra-area transport of O_(3) was significant in polluted circulations(SWW-and C-CTs).In addition,higher temperature,radiation and less rainfall also contributed to higher O_(3) in northern Beijing under the SWW type.For the clean CTs(AN and ESN CTs),precursor amount and intra-area transport played a dominant role in O_(3) distribution.Under the northeasterly low-pressure CT,better formation conditions and higher precursor amount combined with the intra-area southerly transport to cause higher O_(3) values in the south than in the north.The higher O_(3) in the northwestern area under the northeasterly high-pressure type was influenced by weaker titration loss and high O_(3) concentration in previous day.Annual variation in the CTs contributed up to 86.1%of the annual variation in O_(3).About 78%-83%of the diurnal variation in O_(3) resulted from local meteorological factors.
文摘西藏尼木地区分布一套增生杂岩,其对冈底斯火山岩浆弧的演化具有重要意义。本文对该套增生杂岩中的变质火山岩的地质特征、矿物学、全岩地球化学和锆石U-Pb年代学等方面进行了综合研究。变质火山岩以斜长角闪岩、角闪斜长片麻岩为主,其中,角闪石主要为镁质角闪石,共生的斜长石主要为拉长石;变质火山岩经历了高温-中压变质作用;岩石富Al 2 O 3和贫TiO 2,弱富集轻稀土元素(LREE),富集Rb、Sr、Ba等大离子亲石元素(LILE),亏损Nb、Ta、Ti等高场强元素(HFSE),其地球化学特征与火山弧玄武岩的地球化学特征相似,其形成的构造环境为洋内岛弧或活动大陆边缘弧;岩浆锆石U-Pb年龄值为151.4±1.6Ma和150.7±1.4Ma,表明岩石的形成时代为晚侏罗世。综合研究认为,增生杂岩中的变质火山岩是新特提斯洋在晚侏罗世北向俯冲的产物,在陆-陆碰撞之前卷入增生系统,该套变质火山岩不是以往所认为的变质结晶基底。
