发达国家生态发展道路的比较与透视

＂先污染、后治理＂是发达国家生态发展道路的共同特点。在概述发达国家生态发展道路演变历程的基础上,对其进行历史比较,总结出欧盟、美国和日本在生态发展道路上的不同特征,并对欧、美、日生态发展道路的内涵和本质进行分析,从而提出中国在生态发展中应该注意的问题：借鉴发达国家的生态治理经验,在科学发展观的指导下,采用以绿色城市化、绿色空间布局、横向布局与流域开发为基础的新的发展方式,实现具有中国特色的生态文明。     

基于货运车辆GPS数据的交通调查技术研究

基于GPS轨迹点与道路网络拓扑数据,利用GIS技术进行OD点和交通通道的调查研究。利用货运车辆GPS轨迹数据,分析轨迹点的时间、速度及其空间分布特征,实验并确定合理的阈值过滤出点簇,生成OD点;用轨迹点捕获含有拓扑关系的临近路段,通过最短路径算法生成货运车辆沿道路的线型轨迹,最终获得完整的货运车辆出行通道调查数据。与传统交通调查方法相比,该方法的组织实施环节大大减少,调查数据和成果更加客观可靠,是一种通过信息技术进行交通调查研究的全新尝试。     

中国城市化发展质量的综合测度与提升路径

城市化质量是经济城市化质量、社会城市化质量和空间城市化质量的有机统一,城市化发展质量的提升是加快推进我国城市化进程健康发展的关键。本文借助象限图法,通过对城市化质量、速度与城市化水平互动协调关系的分析,从经济、社会、空间三方面提出了由三类指标、12项具体指标组成的城市化发展质量综合测度的三维指标球及判别标准值,引进阿特...     

Construction of a composite pressure–temperature path: revealing the synorogenic burial and exhumation history of the Sevier hinterland, USA

Metamorphic pressure–temperature (P–T) paths derived from 16 growth‐zoned garnets, nine from this study and seven from a previous study, have been combined to construct a detailed composite path for an area in the hinterland of the Cretaceous to early Tertiary Sevier orogenic belt in southern Idaho and north‐west Utah. Samples are from two Proterozoic units in the footwall of the Basin‐Elba thrust: the schist of Mahogany Peaks in the central Albion Mountains, Idaho, and the schist of Stevens Spring in the Basin Creek area of the Grouse Creek Mountains, Utah, ～40 km to the south. The simulated portions of the garnets analysed in this study grew from reactions involving the breakdown of chlorite in the upper greenschist to lower amphibolite facies. Multiple garnets were analysed from three samples. Overlapping segments of P–T paths from different garnets in the same sample correlate with respect to slope and garnet Mn concentration. The composite P–T path documents three episodes of sharply increasing pressures separated by two episodes of pressure decrease, all during progressively increasing temperatures. The path is interpreted to represent alternating episodes of synconvergent thrusting and extensional exhumation in the hinterland of the Sevier orogen. Burial was probably caused by the Basin‐Elba fault, the only major thrust exposed in the region. Extensional exhumation may have occurred along the Mahogany Peaks or Emigrant Spring faults, or by extensional reactivation of the Basin‐Elba fault. This method of correlating partial P–T paths to reveal a more complete composite path provides a powerful tool in unveiling orogenic histories in metamorphic terranes, where evidence of major structures responsible for burial and exhumation is commonly obscured by later events.     

马氏珠母贝经济性状对体重决定效应分析

采用通径分析方法研究了不同养殖区马氏珠母贝各分性状对体重的决定效应。结果表明:流沙养殖群体分性状壳长、壳高、壳宽、铰合线长、软体部重和闭壳肌重与体重间呈正相关(P<0.01),对体重的直接决定效应分别为0.091、0.072、0.029、0.002、0.089和0.001,间接决定效应分别为0.319、0.284、0.183、0.03、0.304和0.004,总决定效应分别为0.41、0.356、0.212、0.032、0.393和0.005;6个经济性状与体重间的关系在抽样断面上可用线性回归模型拟合,复相关系数达0.939(P<0.01)。6个性状3类决定效应按大小排列均为壳长>软体部重>壳宽>壳高>铰合线长>闭壳肌重。迈陈养殖群体作为验证群体,各效应值与前者有差异,但3类决定效应大小排序与前者完全相同。基于决定效应大小及性状易测性,育种目标性状的选择策略为首选壳长,二选壳高,三选壳宽。研究还发现壳宽对软体部重具有最大的决定效应,提出加大壳宽选择强度以培育大型珍珠新观点。     

Cloud Properties and Its Relation to Precipitation over Northwest China

The temporal and spatial distribution of cloud properties over Northwest China has been analyzed using the ISCCP (International Satellite Cloud Climatology Project) monthly mean D2 data from July 1983 to September 2001. The result shows that the regional average total cloud amount, optical thickness, and water path are 52.5%-58.3%, 2.6-6.6, and 44.9-77.6 g m-2, respectively. The major feature of spatial distribution is that higher value areas of cloud properties are all over Tianshan, Kunlun, and Qilian Mountains, while the lower values of cloud properties are over Tarim Basin, the western desert of Inner Mongolia, and the northwestern part of the Loess Plateau. The higher values of cloud amounts are generally associated with higher level of precipitation. For example, the amounts of stratiform clouds with large water path values are good consistent with precipitation. But the amounts of cumuliform and stratocumuliform clouds do not have de nite relation to precipitation.     

Hillslope‐swamp interactions and flow pathways in a hypermaritime rainforest,British Columbia

The process of water delivery to a headwater stream in a hypermaritime rainforest was examined using a variety of physical techniques and tracing with dissolved organic carbon (DOC) and the stable isotopes of water. Headwater swamps, often the major discharge zones for water draining off steep forest slopes, strongly affect the physical and chemical character of streamflow in the region. The headwater swamp selected for detailed investigation was sustained by relatively constant groundwater input from the steep colluvial slopes that maintained the water table above the ground surface. During significant storm events the water table rose quickly and the swamp expanded to engulf marginal pools that developed rapidly on the adjacent ground surfaces. The corresponding release of surface water directly to the stream typically comprised up to 95% of total stream discharge. The proportion of groundwater seepage to the stream by matrix flow (<1%) and via macropore‐fed springs (up to 73%) increased during the recession period, but could not be sustained over the longer term. In more protracted drying periods, deep groundwater contributions to the stream were routed first to the headwater swamp. Dissolved organic carbon (DOC) in the stream, measured daily or more frequently during storm events, was found to be directly proportional to discharge, owing to the domination of DOC‐rich headwater‐swamp water sources. Although δ¹⁸O and δ²H composition of rainwater, groundwater and stream flow were found to be similar, deuterium excess (d ? δ²H ? 8δ¹⁸O) of water components was often found to be distinct, and suggested short water residence times of roughly 12 days for one event. Overall, observations of a typical headwater swamp reveal that the groundwater regime is dominated by rapid infiltration and short, emergent flow paths. With a relatively short turnover time, potential disturbances to the system by harvesting of upslope areas can be expected to occur rapidly. Forest managers can mitigate some of the harmful effects of logging operations by respecting the integrity of headwater wetland systems. The nature and magnitude of such perturbations will require further study. Copyright © 2003 John Wiley & Sons, Ltd.     

Proterozoic low-pressure/high-temperature metamorphism and an anticlockwise P–T–t path for the Hazeldene area, Mount Isa Inlier, Queensland, Australia

In the Hazeldene area, situated in the Mount Isa Inlier, Queensland, the metamorphic grade changes from chlorite zone, through biotite and cordierite zones, to sillimanite/K-feldspar zone.
Microstructural studies of rocks near the sillimanite isograd demonstrate that cordierite grew early during the development of a steep foliation (S2), was replaced by biotite, andalusite and sillimanite at the metamorphic peak late in S2, and in turn by kyanite + chlorite adjacent to localized small post-D2 shear zones. Although the anticlockwise P–T–t path is well defined, the precise P–T conditions are uncertain because of problems with experimental and thermodynamic data. The best estimate for the metamorphic peak for rocks close to the sillimanite isograd is around 600° C at 4 kbar.
The metamorphism has been dated at 1544 Ma, and was synchronous with a major crustal shortening event. Because proposed extensional events occurred more than 60 Ma earlier, their contribution to the peak metamorphic thermal perturbation would have been insignificant. The syn-metamorphic Mica Creek Pegmatites, the abundance of high heat-producing elements in the nearby pre-D2 Sybella Granite, and advective heat by fluids which caused considerable metasomatism in the Hazeldene area, may have each contributed to the thermal budget. However, the metamorphic thermal gradient may be 80°C km^-1 or higher, strongly suggesting a local magmatic control. As none are known in the area, such syn-metamorphic plutons would have to lie beneath the exposed high-grade rocks.     

An example of ultrahigh-temperature metamorphism: orthopyroxene–sillimanite–garnet, sapphirine–quartz and spinel–quartz parageneses in Al–Mg granulites from In Hihaou, In Ouzzal, Hoggar

Quartz Al–Mg granulites exposed at In Hihaou, In Ouzzal (NW Hoggar), preserve an unusual high-grade mineral association stable at temperatures up to 1050°C, involving the parageneses orthopyroxene–sillimanite–garnet–quartz, sapphirine–quartz and spinel–quartz. The phase relationships within the FMAS system show that a continuum exists between the earlier prograde reaction textures and those of the later decompressive event. The following mineral reactions involving sillimanite are deduced: (1) Grt+Qtz→Opx+Sil, (2) Opx+Sil→Grt+Spr+Qtz, (3) Grt+Sil+Qtz→Crd, (4) Grt+Sil→Crd+Spr, (5) Grt+Sil+Spr→Crd+Spl, (6) Grt+Sil→Crd+Spl, (7) Grt+Crd+Sil→Spl+Qtz and (8) Grt+Sil→Spl+Qtz. Minerals in quartz Al–Mg granulites display compositional variations consistent with the observed reactions. The Mg/(Mg+Fe²⁺) range of the main minerals is as follows: cordierite (0.81–0.97), sapphirine (0.77–0.88), orthopyroxene (0.65–0.81), garnet (0.33–0.64) and spinel (0.23–0.56). The reaction textures and the evolution of the mineral assemblages in the quartz Al–Mg granulites indicate a clockwise P–T trajectory characterized by peak conditions of at least 10 kbar and 1050°C, followed by decompression from 10 to 6 kbar at a temperature of at least 900°C.