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401.
柿竹园夕卡岩中有早、晚形成的两种产状石榴子石。本文为查明其形成物理化学条件及与矿化的关系,采用矿区天然花岗岩、灰岩和夕卡岩化早期形成的石榴子石为试样进行了模拟实验研究。实验结果表明:夕卡岩化早期石榴子石是在温度400—750℃,压力500—1000bar,pH=5—8条件下,由富含Si、Al、Fe、Cl、F等组分的热液与上泥盆统佘田桥组灰岩交代反应形成的;晚期石榴子石是在温度250—700℃,压力500—1000bar,pH=5—14条件下,由富含Si、Al、F等组分的带钨溶液与早期石榴子石交代反应产生重结晶作用形成的。 相似文献
402.
This paper deals with the method of bearing test on dynamic compacted bases and the characteristics of the bases. The test results show that the bases have two-stratum structures. For this reason, attentions must be paid to distribute locations of the test at different depths and to do some computer verifications for the underlying soft stratum. 相似文献
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本文所述长江河口地区,指河口附近的陆上部分,包括北部的三角洲平原,东部的滨海平原及西南部的冲积一湖积平原。全区除局部见有一些基岩山体以外,绝大部分为第四系覆盖区。整个第四系岩相层序比较复杂,反映沉积环境有过多次更替。 相似文献
408.
T. Wang H. Guo D. R. Blake Y. H. Kwok I. J. Simpson Y. S. Li 《Journal of Atmospheric Chemistry》2005,52(3):295-317
We present a 16-month record of ozone (O3), carbon monoxide (CO), total reactive nitrogen (NOy), sulphur dioxide (SO2), methane (CH4), C2 – C8 non-methane hydrocarbons (NMHCs), C1 – C2 halocarbons, and dimethyl sulfide (DMS) measured at a southern China coastal site. The study aimed to establish/update seasonal
profiles of chemically active trace gases and pollution tracers in subtropical Asia and to characterize the composition of
the `background' atmosphere over the South China Sea (SCS) and of pollution outflow from the industrialized Pearl River Delta
(PRD) region and southern China. Most of the measured trace gases of anthropogenic origin exhibited a winter maximum and a
summer minimum, while O3 showed a maximum in autumn which is in contrast to the seasonal behavior of O3 in rural eastern China and in many mid-latitude remote locations in the western Pacific. The data were segregated into two
groups representing the SCS background air and the outflow of regional continental pollution (PRD plus southern China), based
on CO mixing ratios and meteorological conditions. NMHCs and halocarbon data were further analyzed to examine the relationships
between their variability and atmospheric lifetime and to elucidate the extent of atmospheric processing in the sampled air
parcels. The trace gas variability (S) versus lifetime (τ) relationship, defined by the power law, Slnx = Aτ− b, (where X is the trace gas mixing ratio) gives a fit parameter A of 1.39 and exponent b of 0.42 for SCS air, and A of 2.86 and b of 0.31 for the regional continental air masses. An examination of ln[n-butane]/ln[ethane] versus ln[propane]/ln[ethane] indicates that their relative abundance was dominated by mixing as opposed
to photochemistry in both SCS and regional outflow air masses. The very low ratios of ethyne/CO, propane/ethane and toluene/benzene
suggest that the SCS air mass has undergone intense atmospheric processing since these gases were released into the atmosphere.
Compared to the results from other polluted rural sites and from urban areas, the large values of these species in the outflow
of PRD/southern China suggest source(s) emitting higher levels of ethyne, benzene, and toluene, relative to light alkanes.
These chemical characteristics could be unique indicators of anthropogenic emissions from southern China. 相似文献
409.
位于青藏高原东北缘的多福屯第三纪火山岩,为钠质基性火山岩系。该火山岩(La/Yb)N值在6—11,∑REE平均为117,样品普遍具有不相容元素富集、Pb亏损以及弱的Nb、Ta正异常,Nb/U和Ce/Pb平均值分别为30和17;样品的87^Sr/^86Sr值为0.7041~O.7069,Nd初始值为0.5129(εNd(t)=6),△^207Pb/^240Pb和△^208Pb/^204Pb分别在11~19和73-84之间,结合高的Sr初始值,表现了特征的Dupal(高放射成因铅)异常。地球化学特征表明,该火山岩属于似OIB性质的陆内火山岩,源区具有DM与EMⅡ混合特点。个别岩石表现出明显陆壳混染的迹象。火山岩源区特征反映了OIB类岩石的复杂性,可能由区域原、古特提斯地幔继承而来,因而是原地的和固有的,并非与青藏高原物质向东挤出有关。通过与邻区同时代火山岩的对比推断,整个高原东北缘新生代火山岩幔源区具有小尺度的不均一性。高原东北缘新生代火山岩的发育可能与较大规模的贺兰-川滇南北复合构造有关。 相似文献
410.
Vertical migration of municipal wastewater in deep injection well systems,South Florida,USA 总被引:1,自引:2,他引:1
Deep well injection is widely used in South Florida, USA for wastewater disposal largely because of the presence of an injection zone (“boulder zone” of Floridan Aquifer System) that is capable of accepting very large quantities of fluids, in some wells over 75,000 m3/day. The greatest potential risk to public health associated with deep injection wells in South Florida is vertical migration of wastewater, containing pathogenic microorganisms and pollutants, into brackish-water aquifer zones that are being used for alternative water-supply projects such as aquifer storage and recovery. Upwards migration of municipal wastewater has occurred in a minority of South Florida injection systems. The results of solute-transport modeling using the SEAWAT program indicate that the measured vertical hydraulic conductivities of the rock matrix would allow for only minimal vertical migration. Fracturing at some sites increased the equivalent average vertical hydraulic conductivity of confining zone strata by approximately four orders of magnitude and allowed for vertical migration rates of up 80 m/year. Even where vertical migration was rapid, the documented transit times are likely long enough for the inactivation of pathogenic microorganisms. 相似文献