Studies of phosphazenes. Part 33. Thermal rearrangement of alkoxy(p-methylphenoxy)cyclophosphazenes: a synthetic route to oxocyclophosphazanes, phosphazadienes and phosphaz-1-enes

The aryloxy(alkoxy)cyclotriphosphazenes N3P3(OR)6��¿½m(OC6H4Me-p)n(R = Me, n= 1�3; R = Et or CH2Ph, n= 3) rearrange on heating to give trioxocyclotriphosphazanes; the di- and mono-methoxy derivatives, N3P3(OMe)6��¿½n(OC6H4Me-p)n(n= 4 or 5), yield dioxophosphaz-1-enes and an oxophosphazadiene respectively. The 1H, 13C and 31P NMR data for the starting materials and the products are presented. No evidence has been found for partially rearranged products. The geometrical disposition of the aryloxy groups in the starting material is retained in the rearranged products. Some aspects of the mechanism of the thermal rearrangement are discussed.

Neoarchean arc magmatism followed by high-temperature, high-pressure metamorphism in the Nilgiri Block, southern India

The Nilgiri Block, southern India is an exhumed lower crust formed through arc magmatic processes in the Neoarchean. The main lithologies in this terrane include charnockites, gneisses, volcanic tuff, metasediments, banded iron formation and mafic-ultramafic bodies. Mafic-ultramafic rocks are present towards the northern and central part of the Nilgiri Block. We examine the evolution of these mafic granulites/metagabbros by phase diagram modeling and U-Pb sensitive high resolution ion microprobe (SHRIMP) dating. They consist of a garnet-clinopyroxene-plagioclase-hornblende-ilmenite +/- orthopyroxene +/- rutile assemblage. Garnet and clinopyroxene form major constituents with labradorite and orthopyroxene as the main mineral inclusions. Labradorite, identified using Raman analysis, shows typical peaks at 508 cm(-1), 479 cm(-1), 287 cm(-1) and 177 cm(-1). It is stable along with orthopyroxene towards the low-pressure high-temperature region of the granulite fades (M1 stage). Subsequently, orthopyroxene reacted with plagioclase to form the peak garnet + clinopyroxene + rutile assemblage (M2 stage). The final stage is represented by amphibolite facies-hornblende and plagioclase-rim around the garnet-clinopyroxene assemblage (M3 stage). Phase diagram modeling shows that these mafic granulites followed an anticlockwise P-T-t path during their evolution. The initial high-temperature metamorphism (M1 stage) was at 850-900 degrees C and similar to 9 kbar followed by high-pressure granulite fades metamorphism (M2 stage) at 850-900 degrees C and 14-15 kbar. U-Pb isotope studies of zircons using SHRIMP revealed late Neoarchean to early paleoproterozoic ages of crystallization and metamorphism respectively. The age data shows that these mafic granulites have undergone arc magmatism at ca. 25392 +/- 3 Ma and high-temperature, high-pressure metamorphism at ca. 2458.9 +/- 8.6 Ma. Thus our results suggests a late Neoarchean arc magmatism followed by early paleoproterozoic high-temperature, high-pressure granulite facies metamorphism due to the crustal thickening and suturing of the Nilgiri Block onto the Dharwar Craton. (C) 2015 Elsevier B.V. All rights reserved.

An Algebraic Preservation Theorem for Aleph-Zero Categorical Quantified Constraint Satisfaction

23 p. -- An extended abstract of this work appears in the proceedings of the 2012 ACM/IEEE Symposium on Logic in Computer Science

The COMT Val158 Met polymorphism as an associated risk factor for Alzheimer disease and mild cognitive impairment in APOE 4 carriers

Background: The aim of this study is to examine the influence of the catechol-O-methyltranferase (COMT) gene (polymorphism Val158 Met) as a risk factor for Alzheimer's disease (AD) and mild cognitive impairment of amnesic type (MCI), and its synergistic effect with the apolipoprotein E gene (APOE). A total of 223 MCI patients, 345 AD and 253 healthy controls were analyzed. Clinical criteria and neuropsychological tests were used to establish diagnostic groups. The DNA Bank of the University of the Basque Country (UPV-EHU) (Spain) determined COMT Val158 Met and APOE genotypes using real time polymerase chain reaction (rtPCR) and polymerase chain reaction (PCR), and restriction fragment length polymorphism (RFLPs), respectively. Multinomial logistic regression models were used to determine the risk of AD and MCI. Results: Neither COMT alleles nor genotypes were independent risk factors for AD or MCI. The high activity genotypes (GG and AG) showed a synergistic effect with APOE epsilon 4 allele, increasing the risk of AD (OR = 5.96, 95% CI 2.74-12.94, p < 0.001 and OR = 6.71, 95% CI 3.36-13.41, p < 0.001 respectivily). In AD patients this effect was greater in women. In MCI patients such as synergistic effect was only found between AG and APOE epsilon 4 allele (OR = 3.21 95% CI 1.56-6.63, p = 0.02) and was greater in men (OR = 5.88 95% CI 1.69-20.42, p < 0.01). Conclusion: COMT (Val158 Met) polymorphism is not an independent risk factor for AD or MCI, but shows a synergistic effect with APOE epsilon 4 allele that proves greater in women with AD.

Regional variations in upper mantle structure beneath North America

Several types of seismological data, including surface wave group and phase velocities, travel times from large explosions, and teleseismic travel time anomalies, have indicated that there are significant regional variations in the upper few hundred kilometers of the mantle beneath continental areas. Body wave travel times and amplitudes from large chemical and nuclear explosions are used in this study to delineate the details of these variations beneath North America.

As a preliminary step in this study, theoretical P wave travel times, apparent velocities, and amplitudes have been calculated for a number of proposed upper mantle models, those of Gutenberg, Jeffreys, Lehman, and Lukk and Nersesov. These quantities have been calculated for both P and S waves for model CIT11GB, which is derived from surface wave dispersion data. First arrival times for all the models except that of Lukk and Nersesov are in close agreement, but the travel time curves for later arrivals are both qualitatively and quantitatively very different. For model CIT11GB, there are two large, overlapping regions of triplication of the travel time curve, produced by regions of rapid velocity increase near depths of 400 and 600 km. Throughout the distance range from 10 to 40 degrees, the later arrivals produced by these discontinuities have larger amplitudes than the first arrivals. The amplitudes of body waves, in fact, are extremely sensitive to small variations in the velocity structure, and provide a powerful tool for studying structural details.

Most of eastern North America, including the Canadian Shield has a Pn velocity of about 8.1 km/sec, with a nearly abrupt increase in compressional velocity by ~ 0.3 km/sec near at a depth varying regionally between 60 and 90 km. Variations in the structure of this part of the mantle are significant even within the Canadian Shield. The low-velocity zone is a minor feature in eastern North America and is subject to pronounced regional variations. It is 30 to 50 km thick, and occurs somewhere in the depth range from 80 to 160 km. The velocity decrease is less than 0.2 km/sec.

Consideration of the absolute amplitudes indicates that the attenuation due to anelasticity is negligible for 2 hz waves in the upper 200 km along the southeastern and southwestern margins of the Canadian Shield. For compressional waves the average Q for this region is > 3000. The amplitudes also indicate that the velocity gradient is at least 2 x 10^-3 both above and below the low-velocity zone, implying that the temperature gradient is &#60; 4.8°C/km if the regions are chemically homogeneous.

In western North America, the low-velocity zone is a pronounced feature, extending to the base of the crust and having minimum velocities of 7.7 to 7.8 km/sec. Beneath the Colorado Plateau and Southern Rocky Mountains provinces, there is a rapid velocity increase of about 0.3 km/sec, similar to that observed in eastern North America, but near a depth of 100 km.

Complicated travel time curves observed on profiles with stations in both eastern and western North America can be explained in detail by a model taking into account the lateral variations in the structure of the low-velocity zone. These variations involve primarily the velocity within the zone and the depth to the top of the zone; the depth to the bottom is, for both regions, between 140 and 160 km.

The depth to the transition zone near 400 km also varies regionally, by about 30-40 km. These differences imply variations of 250 °C in the temperature or 6 % in the iron content of the mantle, if the phase transformation of olivine to the spinel structure is assumed responsible. The structural variations at this depth are not correlated with those at shallower depths, and follow no obvious simple pattern.

The computer programs used in this study are described in the Appendices. The program TTINV (Appendix IV) fits spherically symmetric earth models to observed travel time data. The method, described in Appendix III, resembles conventional least-square fitting, using partial derivatives of the travel time with respect to the model parameters to perturb an initial model. The usual ill-conditioned nature of least-squares techniques is avoided by a technique which minimizes both the travel time residuals and the model perturbations.

Spherically symmetric earth models, however, have been found inadequate to explain most of the observed travel times in this study. TVT4, a computer program that performs ray theory calculations for a laterally inhomogeneous earth model, is described in Appendix II. Appendix I gives a derivation of seismic ray theory for an arbitrarily inhomogeneous earth model.

Fragilidade e desempenho cognitivo em idosos clientes de uma operadora de saúde da zona norte da cidade do Rio de Janeiro

Alguns autores entendem o declínio cognitivo como fator de risco para fragilidade. No entanto, outros estudos apresentam a fragilidade como fator de risco para declínio cognitivo. O presente estudo também entende a relação entre fragilidade e desempenho cognitivo neste sentido. Ainda são poucos os estudos que avaliaram esta associação na literatura internacional e não identificamos nenhum estudo conduzido no Brasil, ou mesmo na América Latina, que a tenha investigado. Este estudo tem como objetivo, investigar a associação entre a síndrome da fragilidade e desempenho cognitivo em idosos, e o efeito da escolaridade e da idade nesta associação. Para isto, analisaram-se dados seccionais da Fase 1 do Estudo da fragilidade em Idosos Brasileiros (Rede FIBRA - Fragilidade em Idosos Brasileiros), relativos à clientes de uma operadora particular de saúde, com 65 anos ou mais, residentes na zona norte da cidade do Rio de Janeiro. A população final de estudo foi de 737 idosos. O desempenho cognitivo foi avaliado através do Mini Exame do Estado Mental (MEEM). Foram considerados frágeis os indivíduos que apresentaram três ou mais das seguintes características: perda de peso não intencional (mais de 4,5Kg no último ano); sensação de exaustão auto-relatada; baixo nível de força de preensão palmar (sujeitos no primeiro quintil); baixo nível de atividade física (sujeitos no primeiro quintil do Minnesota) e lentifica��ão da marcha (sujeitos no primeiro quintil). Também foram coletadas informações sobre características socioeconômicas e demográficas, apoio social, condições médicas e capacidade funcional. O desempenho cognitivo (MEEM) e a fragilidade foram analisados como variáveis dicotômicas. Avaliou-se o papel da idade e escolaridade como possíveis modificadoras de efeito na associação entre fragilidade e baixo desempenho cognitivo. A avaliação da associação entre fragilidade e desempenho cognitivo foi feita através de regressão logística multivariada. A variável idade se comportou como modificadora de efeito na associação entre fragilidade e desempenho cognitivo, x(5) = 806,97, p<0,0001. O mesmo não ocorreu com a variável escolaridade. Os idosos frágeis apresentaram uma maior prevalência de baixo desempenho cognitivo, quando comparados aos idosos não-frágeis ou pré-frágeis, nos três estratos estudados (65 a 74 anos;75 a 84 anos; >_85 anos), p<0,001. A associação entre fragilidade e baixo desempenho cognitivo foi encontrada somente em idosos com 75 anos ou mais, sendo OR bruto=2,68 (IC 95% 1,29 5,53) para idosos de 75 a 84 anos e OR bruto= 6,39 (IC 95% 1,82 - 22,42) para idosos de 85 anos ou mais. Após ajuste pelas condições de saúde, capacidade funcional e pelas variáveis socioeconômicas e demográficas, a associação entre fragilidade e baixo desempenho cognitivo se manteve nesses estratos, OR aj=2,78 (IC 95% 1,23 - 6,27) para 75 a 84 anos e OR aj=15,62 (IC 95% 2,20 110,99) para 85 anos ou mais. A síndrome da fragilidade está, portanto, associada ao baixo desempenho cognitivo em idosos. A idade revelou-se como modificadora de efeito nesta associação. Os idosos com idade mais avançada revelaram uma associação mais expressiva entre os dois fenômenos.

Estudo das alterações cardiovasculares e metabólicas em modelo experimental de programação metabólica: efeito de extrato da casca de uva Vitis vinífera

Estudos epidemiológicos e experimentais têm sugerido que fatores de risco cardiovasculares podem ser parcialmente atribuídos às influências do ambiente em que vive o indivíduo, e que a nutrição materna influencia na programação de alterações metabólicas e cardiovasculares no indivíduo adulto e que caracterizam a síndrome metabólica (SM). Em contrapartida, estudos prévios de nosso laboratório demonstram que o extrato da casca de uva Vitis labrusca (GSE) possui efeito vasodilatador, antihipertensivo e antioxidante. Desta forma, o objetivo deste estudo foi avaliar o efeito do tratamento oral com GSE (200mg/kg/dia), sobre as alterações cardiovasculares e metabólicas e estresse oxidativo observados na prole adulta (fêmea e machos) com 3 e 6 meses, cujas mães foram submetidas a uma dieta rica em gordura (hiperlipídica) durante a lactação. Quatro grupos de ratas foram alimentados com dietas experimentais: controle (7% de gordura); controle + GSE (7% de gordura + GSE), hiperlipídica (24% de gordura); hiperlipídica + GSE (24% de gordura + GSE) durante a lactação. Após o desmame, todos os filhotes passaram a ser alimentados com uma dieta controle e foram sacrificados aos 3 ou 6 meses de idade. A pressão arterial sistólica (PAS) foi medida por pletismografia de cauda e o efeito vasodilatador da acetilcolina (ACh) foi avaliado em leito arterial mesentérico (LAM) perfundido. Foram avaliados o peso corporal, adiposidade (intra-abdominal e gonadal), níveis plasmáticos de colesterol total, triglicerídeos, glicose e insulina, e a resistência à insulina (RI) foi calculada pelo índice de HOMA IR. As expressões do IRS-1, Akt e GLUT-4 foram determinadas em músculo soleus. O dano oxidativo, níveis de nitritos e a atividade das enzimas antioxidantes: superóxido dismutase, catalase e glutationa peroxidase foram dosados no plasma e homogenato de LAM. A PAS e tecido adiposo foram aumentados nas proles adultas de ambos os sexos e idades do grupo hiperlipídico e revertidos pelo tratamento com o GSE. A resposta vasodilatadora à ACh em LAM não foi diferente entre os grupos de ambos os sexos, mas foram reduzidas com o envelhecimento. Nas proles fêmeas e machos do grupo hiperlipídico também foram observados o aumento dos níveis de triglicerídeos, de glicose e RI em ambas as idades e foram reduzidos pelo GSE. No grupo hiperlipídico houve redução nas expressões de IRS-1, Akt e GLUT-4 e o GSE reverteu estas expressões. Os níveis plasmáticos de malondialdeído estavam aumentados e os níveis de nitrito diminuídos no grupo hiperlipídico, de ambos os sexos e idades e foram revertidos pelo GSE. As atividades das enzimas antioxidantes no plasma e no mesentério foram reduzidas no grupo hiperlipídico e restauradas pelo GSE. Em conclusão, O GSE parece proteger as proles fêmeas e machos, cujas mães foram expostas a uma dieta hiperlipídica durante a lactação, dos fatores de riscos cardiovasculares, proporcionando uma fonte alternativa nutricional para a prevenção da SM.

Beyond Q-Resolution and Prenex Form: a Proof System for Quantified Constraint Satisfaction

We consider the quanti fied constraint satisfaction problem (QCSP) which is to decide, given a structure and a first-order sentence (not assumed here to be in prenex form) built from conjunction and quanti fication, whether or not the sentence is true on the structure. We present a proof system for certifying the falsity of QCSP instances and develop its basic theory; for instance, we provide an algorithmic interpretation of its behavior. Our proof system places the established Q-resolution proof system in a broader context, and also allows us to derive QCSP tractability results.

O peptídeo natriurético tipo B (BNP) como preditor de mortalidade a longo prazo em pacientes com síndrome coronariana aguda sem supradesnível do segmento ST

Fundamentos: Apesar dos conhecimentos adquiridos sobre marcadores preditores de mortalidade na síndrome coronariana aguda (SCA), a capacidade de avaliação a longo prazo permanece desconhecida. O peptídeo natriurético tipo B (BNP) tem sido extensamente utilizado, porém as evidências existentes se restringem ao seguimento de curto e médio prazos. Objetivos: Determinar se o BNP é um preditor independente de mortalidade por todas as causas a longo prazo em pacientes com síndrome coronariana aguda sem supradesnível do segmento ST (SCASSST). Métodos: No período de 1o de Janeiro de 2002 a 31 de Dezembro de 2003, foram selecionados 224 pacientes consecutivos atendidos na sala de emergência com SCASSST. A dosagem do BNP à admissão foi incorporada no protocolo diagnóstico, tendo o seu valor sido correlacionado com a mortalidade ao final do seguimento. Resultados: Os pacientes foram acompanhados por 9,34 anos (mediana), tinham 71,5 anos (intervalo IQ=60,5;79,0) e com predomínio do gênero masculino (62,9%). A hipertensão arterial esteve presente em 82,1% e o diabetes em 23,7%. A angina instável (AI) foi diagnosticada em 52,2% e o infarto agudo do miocárdio sem supradesnível do segmento ST (IAMSSST) em 47,8%. O BNP mediano foi de 81,9 pg/ml (intervalo IQ 22,2; 225). A mortalidade se correlacionou com os quartis crescentes do BNP: 14,3; 16,1; 48,2; e 73,2% (p<0,0001). A curva ROC determinou o BNP=100 pg/ml como o melhor ponto de corte, tendo apresentado área sobre a curva (AUC) de 0,79 (IC 95%=0,72-0,85) e sendo preditor de mortalidade ao final do seguimento: 17,3% vs. 65,0%, p<0,001, RR=3,76 (IC 95%=2,49-5,63). O BNP teve poder prognóstico tanto nos pacientes com (26,7 vs. 71,2%, p<0,001) como nos sem (12,9 vs. 56,8%, p<0,001) alteração da função ventricular, e também conforme o diagnóstico de AI (18,7 vs. 48,6%, p=0,001) e IAMSSST (14,9 vs. 75,0%, p<0,001). Na análise de regressão logística, a idade>72 anos (OR=3,79, IC 95%=1,62-8,86, p=0,002), o BNP≥100 pg/ml (OR=6,24, IC 95%=2,95-13,23, p<0,001) e a taxa de filtração glomerular estimada (TFGE)(OR=0,98, IC 95%=0,97-0,99, p=0.049) foram preditores independentes de mortalidade. Conclusões: O BNP dosado à admissão dos pacientes com SCASSST é um forte e independente preditor de mortalidade a longo prazo.

分子系统学分析平台的建立和应用

分子系统学建立在实验和计算的基础之上。DNA快速测序技术的普及为分子系统学家提供了大量数据，而序列分析技术则是探索数据发现知识的重要工具。在基因组时代，随着大量模式生物完整基因组序列的获得，分子系统学正面临着前所未有的机遇和挑战。一方面，生命之树计划有助于确定新的模式生物和开展相应的基因组计划;另一方面，模式生物的基因组计划有助于阐明它们之间的进化关系和基因组的进化模式。更为重要的是，分子系统学序列分析技术已经发展成为探索与整合基因组数据的强有力工具，从而在生命科学中发挥重要作用。事实上，分子系统学和基因组学的相互渗透正在形成一门崭新的交叉学科——系统发育基因组学。 为了奠定分子系统学研究中信息管理和数据分析工作的坚实基础，我们建立了分子系统发育分析平台。该平台为研究人员提供专业数据库服务和数据分析技术支持，以及相关的网络资源。 分子系统发育分析平台包括了3个专业数据库。第一个是DNA凭证标本数据库。该数据库中的记录包括了7项字段：英文科名、中文科名、物种拉丁名、采集人、采集号、采集地和采集时间。用户可以通过设定单个或多个字段的取值进行检索。截止2004年6���1日，该数据库共包括3491条标本记录。第二个是引物数据库。PCR引物是分子系统学实验的重要条件之一。该数据库中的记录包括3项字段：引物名称、序列内容和退火温度。用户可以通过设定单个或多个字段的取值进行检索。截止2004年6���1日，该数据库共包括170条用于扩增植物细胞核、叶绿体和线粒体基因组DNA序列的引物记录。第三个是生物计算数据库。该数据库为研究人员提供传输和保存序列分析数据和结果文件的服务。 为了确保数据库的安全性和使用性，我们开发了数据库的接口和检索工具，以及系统管理员和用户资格认证程序。通过前者，使用者可以进行数据的上传、下载、管理和检索等操作。而后者则是对不同使用者身份和权限进行设定。管理员的权限高于用户，主要负责本系统的日常维护和管理工作，以及对新增管理员和用户进行资格认证。 分析技术支持旨在帮助用户快速掌握常用的系统发育分析方法，进行有效的数据分析，从复杂的统计学算法和计算机程序中解放出来，将精力集中于计算结果的生物学解释。在该部分中，我们首先简要介绍了常用的分析方法，并且针对分子系统学中的不同问题提供了相应的解决方案。这些问题包括：系统发育重建、替代速率和分歧时间的估计、祖先分布区的重建、性状进化假说的检验、以及密码子水平适应性进化的检测。我们特别强调了似然比检验和贝叶斯推测作为方法论上的重要进展在分子系统学中所发挥的关键作用。本部分还包括大量常用的分子系统学程序或软件包及其快速使用说明和命令模块。下载安装之后，用户即可按照说明使用命令模块进行数据分析。 此外，该平台还提供了一些常用的网络资源地址，如生物信息中心、分子进化和系统发育实验室、专业期刊和相关数据库等。 最后还给出了4个应用实例，即针对特定分子系统学问题的解决方案和初步的分析结果。 第一个例子说明系统发育重建方法的应用。为了确定杨梅科的系统学位置，对6���DNA序列和叶绿体trnL-F区内的间隔性状进行了分析。单个分析表明这6���序列之间在系统学信息上存在显著差异。叶绿体基因组序列的合并分析强烈支持杨梅科和（木麻黄科，（桦木科，核果桦科））的姐妹群关系，而间隔性状的存在能够充分提高其分辨率和支持率。 第二个例子说明如何推测历史生物地理学过程。我们对壳斗目8科25属植物叶绿体基因组的trnL-F、matK、rbcL和atpB的合并序列进行了最大简约分析，得到唯一的最大简约树。基于该系统树和25属植物的地理分布数据，采用扩散－替代分析方法重建了系统树每个节点上的祖先分布区，推测了壳斗目的分布历史。结果表明，壳斗目的历史生物地理学过程由3次替代事件和20次扩散事件组成。其中最重要的替代事件是由于冈瓦纳大陆和劳亚大陆分离所导致的南青冈科及其姐妹群之间的分化。另外，在壳斗科和核心高等金缕梅类中多次发生从欧亚大陆到北美洲、甚至南美洲的平行扩散事件。 第三个例子说明如何估计分歧时间。我们仍然使用扩散－替代分析中所用的最大简约树作为分析的依据，并根据等级制似然比检验确定的最优替代模型对该系统树的支长进行了最大似然优化。似然比检验表明，该系统树不服从分子钟假说。我们以冈瓦纳大陆和劳亚大陆分离的地质事件和5个属的最早化石记录作为标定点，采用罚分似然法在没有分子钟的条件下估计了壳斗目的科间分歧时间。结果表明，绝大多数科间分歧事件都发生在白垩纪。 第四个例子说明如何检测密码子水平的适应性进化。分支间可变选择压力模型的似然比检验表明SARS冠状病毒的S基因在跨种传播过程中发生了正选择。

森林生态系统的养分循环-一个温带落叶阔叶林生态系统的研究

l、有机质和全N在草甸土壤的不同层次之间呈现明显的差异，表现力随着土壤深度的增加，含量逐渐降低。无机N包括NH4+-N和No3--N在土层之闻的差异并没有象全N和有机质那么显著。NH4+-在表面30Cm的土壤中明显高于NO3--N的。全P在各层土壤中的含量差异并不显著，但有效p在三层土壤中表现出明显的差异，表现为随土壤深度的增加而降低。 K、Na、Ca���Mg、Fe和AI等6���金属元素的可交换成分在革甸土壤中的含量除K表现出明显的土层间的差异外，在表层30cm的土壤中并没有明显的随土壤深度变化的趋势。 有机质和全N在东灵山地区主要森林土壤中的含量以0~lOcm土层中的显著高于10~20cm的土层中的。20cm的土层中无机N中也以NH4+-为主，这与草甸土壤中的一致。全p和有效P在两个土层之间的差异并不十分显著，而以0^lOcm土层略高于10～20Cm土层的。 K、Na、Ca���Mg、Fe和AI等6���金属元素的可交换成分在不同土层间的差异以K和Ca���为明显，K和Ca���O—1Ocm的土层中要高于lO-20cm的。 森林土壤中的有机质、全N（包括NH4+-N）、全p（包括有效P)都表现为低于亚高山草甸土壤中的，主要原因是亚高山革甸分布于海拔1800cm至2300m，而主要森林类型则基本分布在海拔120m至1500m，亚高山草甸较为恶劣的气候条件明显不利于有机质的矿化，因而分解速率较低，积聚了较多的有机质．而森林土壤中较低的NH4+-N和有效P则可能是由于森林中旺盛的生命活动，尤其是微生物的活动，而大量被植物和微生物固持，因而，即使在森林土壤中有较高的矿化速率，但仍具有较低的NH4+-N和有效p的含量． 不同类型的森林土壤之间各化学成分并没有发现有明显的变化趋势，即使森林类型差异较大的落叶阔叶林和针叶林之间也并没有发现十分显著的差异，这说明各森林类型土壤之间养分特征的一致性。两种针叶林均为人工林，林龄不超过30，而在这之前推测也是以落叶阔叶林为主，森林土壤在这30年间并没有发生十分明显的变化。 在l100m至I500m之间的各种森林类型的土壤也没有表现出十分明显的与海拔高度的相关性。同一森林土壤在不同时间的采样之间，各化学成分也没有表现出明显的差异。 2、降水引起的树干茎流水分中全N的含量在降水季节的初期的含量略高于大量降水期间的。而在降水季节后期，随着每次降雨量的减少，降水间隔时间的增加，树干茎流中N的含量明显地有很大幅度的升高。NO3-N在树干茎流中的含量也同样受到了降水量的影响，表现在后期也发生显著的升高，但升高的幅度没有全N的大。受到降水量影响的元素还有S。 全p在树干茎流水分中含量随降水时间的变化，在各个树种之间有很大的差异。 其它几种元素的可交换态在茎流水分中的含量以K的含量为最高;其次是S、ca���Mg，AI在所有分析的元素中含量最低。不过，AI在降水初期(6���22日)的取样中，含量在几个树种的茎流水分样品中普遍较高，Ca���Mg也被发现有类似的情形。 穿透雨中全N的含量在降水初期略高于降水中期的，而至降水末期时又略有升高，这种格局与树干茎流水分中的具有一致性。全P、K、Ca���Mg、S．ＡＩ等包括全N及其无视成分与树干茎流中的含量的差异并不显著． 地表径流中的全N含量在去除枯枝落叶层的径流场的变化格局与树干茎流和穿透雨中的较为一致．表明这三者之间存在一定的相关性．但与未去除枯枝落叶层的径流场的径流水分中全N和NO３－Ｎ的含量并不十分一致，全N和NO３－N的含量有时较高． 取自马牙石沟流水堰口的集水区水样中全N和NO３-N的含量均变化在l～3ｍｇ／L之间;而取自南沟流水堰口的集水区水样中的全N和N03-N的含量均在l～2mg／L之间，但在这两者之间并没有十分显著的差异，说明取自两个集水区溪流水分中的全N和N03-N的含量基本一致。 3、通过对三个森林立地乔木层生物量的两次调查（相隔6���），发现尽管以辽东栎为主要优势树种的暖温带落叶阔叶混交林（91- 03）第一次调查的生物量低于辽东栋林（91 - 02）和桦木林（91 - 04)的，但在生长6���后，该立地的乔木层生物量已明显超过桦木林的，其增长速率在三个样地中为最高。 根据两次调查的结果，三个样地中出现的11种乔木树种胸径的增加可以分成两组，第一组包括北京花楸、糠椴、白桦和辽东栎，另一组则由山杨、五角枫、棘皮桦、大叶白蜡、蒙椴、黄花柳和沙涞组成。6���中，第一组树种的胸径增加量在1.O～l.4em之间，而第二组的增量在0.2~O.9cm之间，两者之间具有显著的差异。 常用的生物量预测模型包括两个因子，即胸径(D)和树高(H)。D通常可以实测得到，但H大部分只能估计得到。本研究通过比较6���前后两次树高的实际估测结果，证明用D和H共同建立的模型预测结果可能会产生较大的人为误差，建议改用D的单因子预测模型。 无论是实测结果还是树木年轮分析结果，都表明处于目前径级水平的暖温带地区分布的这几个树种还处在不断生长的过程中，随着年龄的增加，表现为胸径还有很大程度的增加，因为这些树种目前的大径级个体的年平均增加速率大于小径级的． 树木年龄与胸径的相互关系的分析结果表明，树木年龄和胸径可以很好地用饱和模型Y=a-be－ｃｘ来拟合． 4、通过近5年对辽东栎枝条( D<0.5cm)和叶片凋落物分解的观察和分析，发现辽东栎枝条的总失重率达到了43%，分解速率常数k为2.713x10－3／周，而叶的总失重率则可以达到70%，分解速率常数k为6.234xl0-3/周. 枝条分解过程中的有机质含量变化可以分为三种类型，一种是单调上升型的，如蛋白质，其含量从3.5%增加到约6%;-种是单调下降型的，如半纤维素，约从15%降低至7%;另一种则是相对变化不大，如粗纤维（包括纤维素和木质素），粗纤维的含量变化在58％±3%，木质素变化在56%±2.5%，纤维素则变化在1%～3%之间。 用Olson指数方程拟合，结果表明粗纤维、木质素和半纤维素三者的分解以半纤维素为最快，分解速率常数为5.693xl0-3／周，其次是木质素和粗纤维，分别为2.461x10-3/周和2.352xl0-3／周．而蛋白质和纤维素的拟合结果较差或根本无法拟合． 用Olsoｎ指数方程拟合的结果表明，有些元素在凋落物分解过程中可以很好地用该方程拟合，如K，Na、Mn和C，p和N，Mg，Zn，而一些元素如Ca���Cu没有取得很好的拟合效果。 几种元素在叶片凋落物分解过程过程的丢失速率也以K为最快，其它元素的顺序为，e，N，p，Na，Mn，Mg和Ca���Ca���拟合效果较差），而Cu、Zn也不能很好地用Olson指数方程拟合。 5、根据对东灵山地区6���(199l~1997)的气象观测结果，可得到该地区的年平均降水量和总降水量，用1994年分析的降水中养分含量的数据可以近似计算得东灵山地区每年通过降水进入该暖温带落叶阔叶林生态系统的几种养分输入量。同理可以计算降水输入养分在树干茎流和穿透雨中的分配，还可以计算养分从地表径流中的输出。通过对这几个水分循环的主要环节中养分输入或输出量的计算，发现每年通过降水而进入系统的养分，大部分将积累在系统中，而输出份额只占很小的一部分。 K和Mg两种养分元素在降水通过林冠和树干表面时，将产生大量的淋溶，而Ca���淋溶较小．N、P和AI则产生少量的吸附或吸收。对于S来说，淋溶和吸收或吸附作用相当，或两者都很小。 通过生物量的年平均增量和生物量中的养分含量可以计算得到每年积累在生物量中的养分量即存留量，同理可以计算年凋落物中的养分量、归还量及生物系统从土壤中吸收的养分量，每年养分的存留率．通过以上计算，发现该落叶阔叶林对养分的存留率较低，这可能是由于该落叶阔叶林森林生态系统每年具有较高的养分归还量，对于一些元素来说，还具有较高的淋溶量，尤其是K和Mg．

神农架植被及其生物多样性与垂直分布格局-兼论中国中、北亚热带植被带的划分

本文主要通过样线法和样方法相结合，进行了大量的群落学调查和分析，分别从植物区系、物种多样性的垂直分布格局和森林群落类型三个方面分析了神农架植被的基本特征及其物种多样性，结果表明： 1．神农架地区具有很高的物种丰富度，有高等植物3，479种，隶属于1，010属，202科。 其中，蕨类植物305种，80属，32科;种子植物3，174种，930属，170科，其中裸子植物32种，19属，6���，被子植物3，142种，911属，164科;单子叶植物501种，175属，21科，双子叶植物2，641种，736���，143科。植物区系属的分布区类型中北温带分布型最多，其次为东亚分布、泛热带分布、东亚北美间断分布、旧世界温带分布以及热带亚洲分布。中国特有成分占5.65%，较全国的8.12%低。温热比(温带分布型(8-11)属数与热带分布型(2-7)属数的比值）为1.200，比全国(0.385)高。 调查样方中共出现高等植物784种，隶属于454属，144科，其中蕨类植物41种，32属，16���;种子植物743种，422属，128科，其中裸子植物20种，14属，5科，被子植物723种，408属，123科;单子叶植物86���，58属，11科，双子叶植物637种，350属，112科。属的分布区类型中北温带分布型最多，其次为东亚分布、泛热带分布、东亚北美间断分布、旧世界温带分布以及热带亚洲分布。温热比为1.52，草本层>乔木层>灌木层分别为2.18、1.76���1.14。 2．神农架植被类型多样，具有常绿阔叶林、常绿落叶阔叶混交林、落叶阔叶林、针阔混交林、亚高山针叶林、硬叶常绿阔叶林和亚高山灌丛草甸等自然植被类型。本文，依据乔木物种的重要值将神农架地区的森林植被划分出了69个类型。用Twinspan将调查的森林群落划分为32组，能基本上反映群落间相似的关系。 3．神农架地区具有完整的植被垂直带谱：海拔900 (1300) m以下为常绿阔叶林带;海拔900 (1300) m～1500 (1800)ⅡI为常绿落叶阔叶混交林带;海拔1500 (1800) m-2000 (2200)m为落叶阔叶林带;海拔2000 (2200) m～2400 (2600)m为针阔混交林带：海拔2400 (2600)m以上为亚高山针叶林带。神农架地区植被的垂直带的分化从总体上比较显著，但由于小生境的异质性和人为干扰，垂直带谱又具有一定的模糊性和次生性。南北坡具有一定的差异，但不十分明显，也说明神农架植被的过渡性。 4．神农架物种多样性的垂直分布格局。神农架的物种多样性与海拔的关系，类似于“中间膨胀”规律(mid-altitude bulge)，在中低海拔处生物多样性最高。通过二次多项式回归拟合，得到如下拟合曲线： 1)海拔与总体物种数：y= _14.445x2+ 34.74lx+42.07，Xd=1.203km; 2)海拔与乔木层物种数：y=-6.9707x2+ 21.334x+0.2004，Xdrl.530km; 3)海拔与灌木层物种数：y=-6.1599x2+ 9.9747x+30.991，Xd=0.8 lOkm: 4)海拔与草本层物种数：y= _3.9907x2+ 10.455x+15.35，Xd-1.308km; 5）海拔与乔木层Shannon-Wiener指数：y=_0.3337x2+ 0.9877x+0.2537，Xd' 1.480km; 6)海拔与灌木层Shannon-Wiener指数：y=-0.1938xz+ 0.422lx+1.2103，Xd=1.089km： 7)海拔与草本层Shannon-Wiener指数：y=_0.1072x2+ 0.294lx+0.9954，Xd=1.372km; x为海拔( km)，y为各物种多样性指标，Xd为物种多样性的最大时的海拔。 从这些拟合曲线中可以看出：总体物种多样性在海拔1200m左右的常绿落叶阔叶混交林带最高：乔木层物种多样性在海拔1500m左右的常绿落叶阔叶混交林带与落叶阔叶林的过渡带最高;灌木层物种多样性在海拔800-llOOm左右的常绿阔叶林与常绿落叶阔叶混交林带的过渡带最高;草本层物种多样性在海拔1300-1400m左右的常绿落叶阔叶混交林带最高。 但物种多样性随海拔变化有许多的起伏和波动。这些波动有些反映了群落的垂直带谱随海拔梯度变化的特点，在垂直带谱的过渡区物种多样性往往较高;有些波动反映了一些特殊的生境，有些反映了人为活动的影响，造成了神农架植被的次生性。因此，影响神农架物种多样性垂直分布的因素有：植被本身的性质和特点、过渡带的特点、生境的异质性和人为活动。 5．神农架植被水平地带性的过渡性。海拔1300m以下的植物属的分布区类型的温热比南坡总是比北坡小，而且相差十分显著，反映了神农架作为植被分界线的价值。神农架南坡的基带植被是常绿阔叶林，因此南坡属于中亚热带。北坡的基带植被，虽然也有常绿树种的零星分布，甚至有小块的常绿阔叶林，完全由于小生境所至，分布的主要类型是常绿落叶阔叶混交林，应属于北亚热带。因此，神农架是中、北亚热带重要的过渡地带。神农架地区中北亚热带的具体分界线宜按照分长江干流和汉水的水岭来划界，即猴子石、大窝坑、神农架、神农顶、老君山一线，南坡属于中亚热带，北坡属于北亚热带。 总之，神农架处于我国中、北亚热带的过渡带，具有过渡带的性质，具有很高的物种多样性，拥有完整的植被垂直带谱，具有多种多样的植物群落及其组成的生态系统。而且，具有我国许多特有植物和珍稀濒危保护植物和许多资源植物。因此，神农架植被在我国植被体系中具有重要的地位，是我国生物多样性最丰富的地区之一，是生物多样性保护的关键地区，也应是生物多样性研究的热点地区。 另外，调查分析了黄山和万朝山植被及其物种多样性与垂直分布格局，结果表明： 6���黄山样方中共出现高等植物259种，隶属于263属，110科，其中蕨类植物14种，II属，8科，种子植物345种，152属，105科，其中裸子植物9种，8属，6���，被子植物336���，144属，99科，其中单子叶植物37种，27属，6���，双子叶植物299种，117属，90科。属的分布区类型中北温带分布最多，其次为东亚分布和泛热带分布，再次为东亚北美间断分布、热带亚洲分布以及旧世界温带分布，与神农架和万朝山也较相似，但热带分布的属更多一些。温热比为1.1875，灌木层>草本层>乔木层，分别为1.3818、1.2609和1.2143。 黄山的森林植被类型有针叶林、常绿阔叶林、常绿落叶阔叶混交林、针阔混交林、落叶阔叶林和竹林。Twinspan将调查的森林群落划分为22组，反映群落间相似的关系，比较清楚和适用。依据乔木物种的重要值将森林植被划分出了34个类型。黄山物种多样性的与海拔的关系不十分明显。黄山植被的垂直带谱不是十分明显，将其垂直带谱划分为：海拔1300m(1500m)以下为常绿阔叶林带;海拔1300m(1500m)-1500m(1600m)常绿落叶阔叶混交林 带;1500m(1600m)以上为落叶阔叶林、黄山松林、山地灌木草丛带。垂直带谱在不同坡向上有差别，东、南、西坡的相似性较大，而北坡与其差别较大。 7．万朝山样方中共出现高等植物490种，隶属于339属，124科，其中蕨类植物21种，18属，11科，种子植物469种，321属，113科，其中裸子植物9种，7属，4科，被子植物460种，314属，109科，其中单子叶植物47种，37属，11科，双子叶植物413种，277属，98科。植物属的分布区类型中，北温带分布所占最多，其次为泛热带分布、东亚分布、东亚北美间断分布、旧世界温带分布以及热带亚洲分布，。温热比为1.3366，草本层>乔木层>灌木层，分别为1.5429、1.4063和1.0645。 万朝山的植被类型包括针叶林、落叶阔叶林、针阔混交林和常绿落时阔叶混交林，但没有典型的常绿阔叶林。依据乔木物种的重要值将森林植被划分出了20个类型。万朝山物种多样性与海拔的关系则不十分明显。万朝山的人为干扰比较强，植被的次生性很大，南、北坡物种多样性随海拔升高的起伏较大。

Increased gas production from hydrates by combining depressurization with heating of the wellbore

To extract gas from hydrate reservoirs, it has to be dissociated in situ. This endothermic dissociation process absorbs heat energy from the formation and pore fluid. The heat transfer governs the dissociation rate, which is proportional to the difference between the actual temperature and the equilibrium temperature. This study compares three potential gas production schemes from hydrate-bearing soil, where the radial heat transfer is governing. Cylindrical samples with 40% pore-filling hydrate saturation were tested. The production tests were carried out over 90 min by dissociating the hydrate from a centered miniature wellbore, by either lowering the pressure to 6, 4, or 6 MPa with simultaneous heating of the wellbore to 288 K. All tests were replicated by a numerical simulation. With additional heating at the same wellbore pressure, the gas production from hydrates could, on average, be increased by 1.8 and 3.6 times in the simulation and experiments, respectively. If the heat influx from the outer boundary is limited, a simulation showed that the specific heat of the formation is rapidly used up when the wellbore is only depressurized and not heated. © 2012 American Chemical Society.

Spray drying: An alternative synthesis method for polycationic oxide compounds

Synthesis of polycationic compounds by the spray-drying technique is an interesting alternative in the domain of aqueous precursor synthesis methods. Spray drying yields high quality samples with good reproducibility. The possibility of scaling up for production of large quantities with fast processing time is well established by the commercial availability of powders of various compositions. In this paper, we have discussed the advantages and limitations of this method and demonstrated its interest by synthesizing a few polycationic compounds selected for their attractive properties of thermoelectricity [Bi1.68Ca2Co1.69O 8, La0.95A0.05CoO3 (A=Ca, Sr, Ba)] or magnetoresistance [La0.70A0.30MnO3 (A=Sr, Ba)]. We have confirmed the quality of these samples by reporting their structure, magnetic and transport properties. © 2010 Elsevier Ltd All rights reserved.

Garra rotundinasus, a new species of cyprinid fish (Pisces : Teleostei) from the upper Irrawaddy River basin, China

Garra rotundinasus, a new cyprinid species from the upper Irrawaddy River basin in Yunnan, China, is herein described. It shares with G. gravelyi the presence of a snout having a poorly developed proboscis represented by a truncate area in front of the nostrils, a character distinguishing both from all other Southeast Asian and Chinese congeners. The two species are distinct in coloration, morphometric and meristic characters. The sympatrically occurring G. tengchongensis is very similar to G. rotundinasus in possessing 36-37 perforated lateral line scales, 5 or 6 scales between the anus and anal-fin origin, and an anterior position of the anus (anus to anal distance 32.1-51.8% of pelvic to anal distance). Garra rotundinasus can be differentiated from G. tengehongensis in having a more slender caudal peduncle, a larger disc and no dark central band on the dorsal fin.