Air Flow Land-Sea-Air Interface: Monterey Bay, California - 1971. Annual Report, Part 1, July 1972

Air flow at the land-sea-air interface influences to a large extent the atmospheric conditions that determine the transport, di lution, and trapping of natural and man-made air pollutants in the coastal areas of Monterey Bay and the Salinas Valley. Analysis of the hourly air flow on a daily and monthly basis indicates patterns of stagnation from midnight to noon of the fol lowing day with moderate to strong air flow during period 1300 to 2200. Throughout the year 1971 whenever flow is greater than 5 mph, the prevailing wind direction is onshore and from a westerly direction. Suggestions for urbanization and industrialization are made on the basis of an understanding of the atmospheric conditions which lead to trapping and dispersal of atmospheric waste. (27 page document)

El paisaje vegetal durante la prehistoria reciente en la vertiente mediterránea de Euskal Herria

421 p. (Bibliogr.: 375-421

Complexity of rupture propagation in large earthquakes in relation to tectonic environment

Complexity in the earthquake rupture process can result from many factors. This study investigates the origin of such complexity by examining several recent, large earthquakes in detail. In each case the local tectonic environment plays an important role in understanding the source of the complexity.

Several large shallow earthquakes (M_s > 7.0) along the Middle American Trench have similarities and differences between them that may lead to a better understanding of fracture and subduction processes. They are predominantly thrust events consistent with the known subduction of the Cocos plate beneath N. America. Two events occurring along this subduction zone close to triple junctions show considerable complexity. This may be attributable to a more heterogeneous stress environment in these regions and as such has implications for other subduction zone boundaries.

An event which looks complex but is actually rather simple is the 1978 Bermuda earthquake (M_s ~ 6). It is located predominantly in the mantle. Its mechanism is one of pure thrust faulting with a strike N 20°W and dip 42°NE. Its apparent complexity is caused by local crustal structure. This is an important event in terms of understanding and estimating seismic hazard on the eastern seaboard of N. America.

A study of several large strike-slip continental earthquakes identifies characteristics which are common to them and may be useful in determining what to expect from the next great earthquake on the San Andreas fault. The events are the 1976 Guatemala earthquake on the Motagua fault and two events on the Anatolian fault in Turkey (the 1967, Mudurnu Valley and 1976, E. Turkey events). An attempt to model the complex P-waveforms of these events results in good synthetic fits for the Guatemala and Mudurnu Valley events. However, the E. Turkey event proves to be too complex as it may have associated thrust or normal faulting. Several individual sources occurring at intervals of between 5 and 20 seconds characterize the Guatemala and Mudurnu Valley events. The maximum size of an individual source appears to be bounded at about 5 x 10²⁶ dyne-cm. A detailed source study including directivity is performed on the Guatemala event. The source time history of the Mudurnu Valley event illustrates its significance in modeling strong ground motion in the near field. The complex source time series of the 1967 event produces amplitudes greater by a factor of 2.5 than a uniform model scaled to the same size for a station 20 km from the fault.

Three large and important earthquakes demonstrate an important type of complexity --- multiple-fault complexity. The first, the 1976 Philippine earthquake, an oblique thrust event, represents the first seismological evidence for a northeast dipping subduction zone beneath the island of Mindanao. A large event, following the mainshock by 12 hours, occurred outside the aftershock area and apparently resulted from motion on a subsidiary fault since the event had a strike-slip mechanism.

An aftershock of the great 1960 Chilean earthquake on June 6, 1960, proved to be an interesting discovery. It appears to be a large strike-slip event at the main rupture's southern boundary. It most likely occurred on the landward extension of the Chile Rise transform fault, in the subducting plate. The results for this event suggest that a small event triggered a series of slow events; the duration of the whole sequence being longer than 1 hour. This is indeed a "slow earthquake".

Perhaps one of the most complex of events is the recent Tangshan, China event. It began as a large strike-slip event. Within several seconds of the mainshock it may have triggered thrust faulting to the south of the epicenter. There is no doubt, however, that it triggered a large oblique normal event to the northeast, 15 hours after the mainshock. This event certainly contributed to the great loss of life-sustained as a result of the Tangshan earthquake sequence.

What has been learned from these studies has been applied to predict what one might expect from the next great earthquake on the San Andreas. The expectation from this study is that such an event would be a large complex event, not unlike, but perhaps larger than, the Guatemala or Mudurnu Valley events. That is to say, it will most likely consist of a series of individual events in sequence. It is also quite possible that the event could trigger associated faulting on neighboring fault systems such as those occurring in the Transverse Ranges. This has important bearing on the earthquake hazard estimation for the region.

大气湍流对斜程传输准单色高斯谢尔光束时间相干性的影响

由第一类零阶贝塞尔函数的级数展开推导出波结构函数在任意湍流条件下的近似表达式。由广义惠更斯菲涅耳原理、随高度变化的Hufnagel-Valley湍流廓线模型以及波结构函数在任意湍流条件下的近似表达式,导出了斜程传输时准单色高斯谢尔光束互相干函数的解析式。然后,利用表征光束时间相干性的纵向相干长度(可由互相干函数导出),研究了斜程传输时大气湍流对准单色高斯谢尔光束时间相干性的影响。研究结果表明,准单色高斯谢尔光束的时间相干性在整个斜程传输过程中保持不变。最后,对该结果在物理上给予了定性解释。

Investigation of strong earthquake ground motion

The pattern of energy release during the Imperial Valley, California, earthquake of 1940 is studied by analysing the El Centro strong motion seismograph record and records from the Tinemaha seismograph station, 546 km from the epicenter. The earthquake was a multiple event sequence with at least 4 events recorded at El Centro in the first 25 seconds, followed by 9 events recorded in the next 5 minutes. Clear P, S and surface waves were observed on the strong motion record. Although the main part of the earthquake energy was released during the first 15 seconds, some of the later events were as large as M = 5.8 and thus are important for earthquake engineering studies. The moment calculated using Fourier analysis of surface waves agrees with the moment estimated from field measurements of fault offset after the earthquake. The earthquake engineering significance of the complex pattern of energy release is discussed. It is concluded that a cumulative increase in amplitudes of building vibration resulting from the present sequence of shocks would be significant only for structures with relatively long natural period of vibration. However, progressive weakening effects may also lead to greater damage for multiple event earthquakes.

The model with surface Love waves propagating through a single layer as a surface wave guide is studied. It is expected that the derived properties for this simple model illustrate well several phenomena associated with strong earthquake ground motion. First, it is shown that a surface layer, or several layers, will cause the main part of the high frequency energy, radiated from the nearby earthquake, to be confined to the layer as a wave guide. The existence of the surface layer will thus increase the rate of the energy transfer into the man-made structures on or near the surface of the layer. Secondly, the surface amplitude of the guided SH waves will decrease if the energy of the wave is essentially confined to the layer and if the wave propagates towards an increasing layer thickness. It is also shown that the constructive interference of SH waves will cause the zeroes and the peaks in the Fourier amplitude spectrum of the surface ground motion to be continuously displaced towards the longer periods as the distance from the source of the energy release increases.

O turismo solidário e a redescrição social no Vale do Jequitinhonha-MG

Esta tese estuda o processo da implantação do Programa de Turismo Solidário pelo governo de Minas Gerais no Vale do Jequitinhonha - MG, bem como as características e os significados que o mesmo adquiriu, tanto junto aos moradores das localidades alvo quanto junto aos chamados turistas solidários, e avalia o estado da arte de modos de turismo semelhantes ao que ocorre no Vale, com ênfase em alguns casos nas favelas cariocas. A tese focaliza a apropriação pela população das diretrizes e dos aspectos teórico-metodológicos da proposta desse Programa; a percepção dos moradores em relação ao turismo que ali ocorre; o enquadramento em que os encontros no turismo solidário ocorrem; os significados do turismo solidário; os indicadores do turismo solidário. Traz, de um lado, uma visão abrangente, discutindo questões relacionadas às políticas públicas no campo do turismo, e de outro lado, uma abordagem de caráter etnográfico, relativa ao encontro intersubjetivo entre ―turistas solidários‖ e a população local. A construção da linha argumentativa da tese fundamenta-se nos seguintes pressupostos: as propostas de descentralização por meio da ideia de governança apresentadas pelas políticas públicas que sustentam a ideologia do Programa de Turismo Solidário são ferramentas importantes para o desenvolvimento local; o encontro entre pessoas com diferentes formas de vida, com reconhecimento recíproco entre si, suscita em ambas as partes um alargamento da percepção de mundo e uma possibilidade para redescrição dos sujeitos; o enquadramento em que a interação ocorre e o nível de intimidade entre os participantes influenciam na possibilidade do individuo repensar valores e atitudes. O documentário ―Retrato Brasil‖ filmado durante as pesquisas de campo, foi elaborado na perspectiva de auxiliar na promoção do que é chamado de turismo solidário, entre outras possibilidades.

Um fio de água na serra me encanta mais que o mar: o Vale do Paraíba fluminense e as transformações espaciais cafeeiras

O Vale do Paraíba passou por um conjunto de transformações espaciais guiadas pelo cultivo do café para exportação ao longo do século XIX. A história ambiental sugere que a natureza seja integrada à análise histórica elaborada por estudiosos do passado. Neste sentido, busca-se compreender a dinâmica de interação entre sociedade e ambiente natural através das técnicas utilizadas no cultivo do café no Vale do Paraíba fluminense no século XIX, com o objetivo de analisar os elementos que condicionaram o processo de estruturação desse cultivo no Vale, assim como o impacto dele resultante àquele ambiente natural. Procura-se ainda investigar de que maneira indivíduos daquela sociedade se posicionaram frente às técnicas utilizadas e perceberam as dinâmicas promovidas pela cultura cafeeira ao ambiente natural.

Fios do novelo: crianças negras, educação e trabalho em Vassouras, 1871 a 1910

Nosso trabalho analisa o processo de escolarização de crianças negras em Vassouras, de 1871 a 1910. Intencionamos unir as reflexões do campo da História e da História da Educação, para compreender a organização da sociedade e a inserção da escola nessa cidade, destacando a presença das crianças negras nos bancos escolares. Para conhecer a organização social de Vassouras dialogamos com Raposo (1978) e Stein (1990), dois historiadores cujas obras marcam a história da cidade. Seguindo a mesma trilha, analisamos a produção dos historiadores ligados ao Vale do Paraíba, tais como: Salles (2008), Muaze (2008) e Gomes (2006) para compreender a formação das famílias e seus títulos de nobreza. Também dialogamos com os professores Góes e Florentino (1997) e Mattos (1998) para compreender a formação da família escrava e o significado da liberdade. Na História da Educação destacamos os estudos desenvolvidos por: Gondra e Schueler (2008), que sinalizam que há poucos estudos sobre o processo de escolarização de negros, afrodescendentes e índios no período imperial. Esse quadro apontado pelos autores citados anteriormente já começou a mudar. O estudo de Silva (2000) sobre a escola para meninos negros na Corte foi um dos pioneiros na perspectiva histórica. Igualmente desbravador do campo foi a pesquisa realizada por Barros (2005) sobre o processo de escolarização de negros em São Paulo. Os trabalhos de Fonseca (2002 e 2009) desmistificam a tese de ausência de crianças negras nas escolas das Gerais. Gonçalves (2005) faz um balanço da questão e apresenta novas lacunas em áreas onde ainda não há pesquisas sobre os negros na Educação, entre elas a província do Rio de Janeiro. Este estudo buscou preencher essa lacuna a partir de documentos que se encontravam em diferentes acervos da cidade e do Estado do Rio de Janeiro. Nessas instituições coletamos: pedidos de Soldada, o jornal O Vassourense, verbetes de dicionários tecnológicos de Direito e verbetes do dicionário bibliográfico Velho Sobrinho. Em Vassouras encontramos os Mapas de Frequência Escolar e os Ofícios remetidos ao diretor da Instrução Pública. O processo histórico de educação dos libertos, iniciado com a Lei do Ventre Livre em 1871, em Vassouras pode ser acompanhado pelos Mapas de Frequência Escolar, e esses documentos nos permitem acompanhar até que idade essa criança negra permanecia na escola e também conhecer a sua saída para o mundo do trabalho. O ano de 1910 foi estabelecido para acompanhar o movimento interno, da própria documentação existente nos acervos de Vassouras, que após esse período apresentavam lacunas que dificultavam a montagem de uma série que permitisse uma análise das questões educacionais em paralelo com as questões sociais e econômicas. Adotamos como suporte teórico metodológico o Paradigma Indiciário proposto por Ginzburg (1989), que busca reconstruir as sociedades de tempos pretéritos a partir de vestígios, pistas e indícios presentes nos documentos. Também nos auxiliaram na leitura dos documentos os livros escritos por Elias (1993, 1994, 2000 e 2001), nos quais buscávamos base para ler o mundo das letras e o mundo do trabalho da sociedade vassourense no final do Império e início da República

Fios do novelo: crianças negras, educação e trabalho em Vassouras, 1871 a 1910

Nosso trabalho analisa o processo de escolarização de crianças negras em Vassouras, de 1871 a 1910. Intencionamos unir as reflexões do campo da História e da História da Educação, para compreender a organização da sociedade e a inserção da escola nessa cidade, destacando a presença das crianças negras nos bancos escolares. Para conhecer a organização social de Vassouras dialogamos com Raposo (1978) e Stein (1990), dois historiadores cujas obras marcam a história da cidade. Seguindo a mesma trilha, analisamos a produção dos historiadores ligados ao Vale do Paraíba, tais como: Salles (2008), Muaze (2008) e Gomes (2006) para compreender a formação das famílias e seus títulos de nobreza. Também dialogamos com os professores Góes e Florentino (1997) e Mattos (1998) para compreender a formação da família escrava e o significado da liberdade. Na História da Educação destacamos os estudos desenvolvidos por: Gondra e Schueler (2008), que sinalizam que há poucos estudos sobre o processo de escolarização de negros, afrodescendentes e índios no período imperial. Esse quadro apontado pelos autores citados anteriormente já começou a mudar. O estudo de Silva (2000) sobre a escola para meninos negros na Corte foi um dos pioneiros na perspectiva histórica. Igualmente desbravador do campo foi a pesquisa realizada por Barros (2005) sobre o processo de escolarização de negros em São Paulo. Os trabalhos de Fonseca (2002 e 2009) desmistificam a tese de ausência de crianças negras nas escolas das Gerais. Gonçalves (2005) faz um balanço da questão e apresenta novas lacunas em áreas onde ainda não há pesquisas sobre os negros na Educação, entre elas a província do Rio de Janeiro. Este estudo buscou preencher essa lacuna a partir de documentos que se encontravam em diferentes acervos da cidade e do Estado do Rio de Janeiro. Nessas instituições coletamos: pedidos de Soldada, o jornal O Vassourense, verbetes de dicionários tecnológicos de Direito e verbetes do dicionário bibliográfico Velho Sobrinho. Em Vassouras encontramos os Mapas de Frequência Escolar e os Ofícios remetidos ao diretor da Instrução Pública. O processo histórico de educação dos libertos, iniciado com a Lei do Ventre Livre em 1871, em Vassouras pode ser acompanhado pelos Mapas de Frequência Escolar, e esses documentos nos permitem acompanhar até que idade essa criança negra permanecia na escola e também conhecer a sua saída para o mundo do trabalho. O ano de 1910 foi estabelecido para acompanhar o movimento interno, da própria documentação existente nos acervos de Vassouras, que após esse período apresentavam lacunas que dificultavam a montagem de uma série que permitisse uma análise das questões educacionais em paralelo com as questões sociais e econômicas. Adotamos como suporte teórico metodológico o Paradigma Indiciário proposto por Ginzburg (1989), que busca reconstruir as sociedades de tempos pretéritos a partir de vestígios, pistas e indícios presentes nos documentos. Também nos auxiliaram na leitura dos documentos os livros escritos por Elias (1993, 1994, 2000 e 2001), nos quais buscávamos base para ler o mundo das letras e o mundo do trabalho da sociedade vassourense no final do Império e início da República

Shallow-water benthic habitats of southwest Puerto Rico

This report describes the creation and assessment of benthic habitat maps for shallow-water (<30m) marine environments of the Guánica/Parguera and Finca Belvedere Natural Reserve in southwest Puerto Rico. The objective was to provide spatially-explicit information on the habitat types, biological cover and live coral cover of the region’s coral reef ecosystem. These fine-scale habitat maps, generated by interpretation of 2010 satellite imagery, provide an update to NOAA’s previous digital maps of the U.S. Caribbean (Kendall et al., 2001) for these areas. Updated shallow-water benthic habitat maps for the Guánica/Parguera region are timely in light of ongoing restoration efforts in the Guánica Bay watershed. The bay is served directly by one river, the Rio Loco, which flows intermittently and more frequently during the rainy season. The watershed has gone through a series of manipulations and alterations in past decades, mainly associated with agricultural practices, including irrigation systems, in the upper watershed. The Guánica Lagoon, previously situated to the north of the bay, was historically the largest freshwater lagoon in Puerto Rico and served as a natural filter and sediment sink prior to the discharge of the Rio Loco into the Bay. Following alterations by the Southwest Water Project in the 1950s, the Lagoon’s adjacent wetland system was ditched and drained; no longer filtering and trapping sediment from the Rio Loco. Land use in the Guánica Bay/Rio Loco watershed has also gone through several changes (CWP, 2008). Similar to much of Puerto Rico, the area was largely deforested for sugar cane cultivation in the 1800s, although reforestation of some areas occurred following the cessation of sugar cane production (Warne et al., 2005). The northern area of the watershed is generally mountainous and is characterized by a mix of forested and agricultural lands, particularly coffee plantations. Closer to the coast, the Lajas Valley Agricultural Reserve extends north of Guánica Bay to the southwest corner of the island. The land use practices and watershed changes outlined above have resulted in large amounts of sediment being distributed in the Rio Loco river valley (CWP, 2008). Storm events and seasonal flooding also transport large amounts of sediment to the coastal waters. The threats of upstream watershed practices to coral reefs and the nearshore marine environment have been gaining recognition. Guánica Bay, and the adjacent marine waters, has been identified as a “management priority area” by NOAA’s Coral Reef Conservation Program (CRCP, 2012). In a recent Guánica Bay watershed management plan, several critical issues were outlined in regards to land-based sources of pollution (LBSP; CWP, 2008). These include: upland erosion from coffee agriculture, filling of reservoirs with sediment, in-stream channel erosion, loss of historical Guánica lagoon, legacy contaminants and sewage treatment (CWP, 2008). The plan recommended several management actions that could be taken to reduce impacts of LBSP, which form the basis of Guánica watershed restoration efforts.

Theoretical gain of strained GeSn0.02/Ge1-x-y ' SixSny ' quantum well laser

Using effective-mass Hamiltonian model of semiconductors quantum well structures, we investigate the electronic structures of the Gamma-conduction and L-conduction subbands of GeSn/GeSiSn strained quantum well structure with an arbitrary composition. Our theoretical model suggests that the band structure could be widely modified to be type I, negative-gap or indirect-gap type II quantum well by changing the mole fraction of alpha-Sn and Si in the well and barrier layers, respectively. The optical gain spectrum in the type I quantum well system is calculated, taking into account the electrons leakage from the Gamma-valley to L-valley of the conduction band. We found that by increasing the mole fraction of alpha-Sn in the barrier layer and not in the well layer, an increase in the tensile strain effect can significantly enhance the transition probability, and a decrease in Si composition in the barrier layer, which lowers the band edge of Gamma-conduction subbands, also comes to a larger optical gain.

Dependence of current-voltage characteristics of pseudomorphic AlAs/In0.53Ga0.47As/InAs resonant tunnelling diodes on quantum well widths

This paper studies the dependence of I - V characteristics on quantum well widths in AlAs/In0.53Ga0.47As and AlAs/In0.53Ga0.47As/InAs resonant tunnelling structures grown on InP substrates. It shows that the peak and the valley current density in the negative differential resistance region are closely related with quantum well width. The measured peak current density, valley current densities and peak-to-valley current ratio of resonant tunnelling diodes are continually decreasing with increasing well width.

Anomalous Pressure Behavior of N-Cluster Emissions in GaAs0.973Sb0.022N0.005

Photoluminescence of GaAs0.973Sb0.022N0.005 is investigated at different temperatures and pressures. Both the alloy band edge and the N-related emissions, which show different temperature and pressure dependences, are observed. The pressure coefficients obtained in the pressure range 0-1.4GPa for the band edge and N-related emissions are 67 and 45 meV/GPa, respectively. The N-related emissions shift to a higher energy in the lower pressure range and then begin to redshift at about 8.5 GPa. This redshift is possibly caused by the increase of the X-valley component in the N-related states with increasing pressure.

Photoluminescence studies of type-II self-assembled InAlAs/AlGaAs QDs grown on (311)A GaAs substrate

The photoluminescence (PL) spectra of self-assembled In0.55Al0.45As/Al0.45Ga0.5As quantum dots (QD) grown on (311)A GaAs substrate were measured. The type- I character of PL related to the X valley was verified by excitation power dependence of peak position and the PL spectra under different pressure , which was attributed to the type- II transition from X valley in Al0.5Ga0.5As to heavy holes in In0.55Al0.45As The high energy Gamma -related transition was also observed above 70K and assigned as the transition between Gamma valley and heavy holes in In-0.55 Al0.45As. The X-valley split was discussed to interpret the observed second X-related peak under pressure.

Type I-type II transition of self-assembled In0.55Al0.45As/Al0.5Ga0.5As quantum dots

The photoluminescence (PL) of In0.55Al0.45As/Al0.5Ga0.5As self-assembled quantum dots has been measured at 15 and 80 K under hydrostatic pressure. The lateral size of the dots ranges from 7 to 62 nm. The emissions from the dots with 26, 52 and 62 nm size have a blue shift under pressure, indicating that these quantum dots have the normal type-I structure with lowest conduction band at the Gamma -valley. However, the PL peak of dots with 7 nm diameter moves to lower energy with increasing pressure. It is a typical character for the X-related transition. Then these small dots have a type-II structure with the X-valley as the lowest conduction level. An envelope-function calculation confirms that the Gamma -like exciton transition energy will rise above the X-like transition energy in the In0.55Al0.45As/Al0.5Ga0.5As structure if the dot size is small enough.