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991.
ShouHua Liu ChangLin Chen KeXiu Liu Lin Mu Hui Wang XinRong Wu JianLi Zhang XiaoFeng Duan Jia Gao 《中国科学:地球科学(英文版)》2015,58(12):2279-2288
A modified Gauss-Markov model with weighted constraints was constructed by combining satellite altimeter and tide gauge records. Vertical motion rates of nine tide gauge stations around the Bohai Sea and Yellow Sea are estimated. This is the first time systematic estimates have been derived in this region. Downward trends were seen at the six tide gauge stations located at Tanggu, Longkou, Laohutan, Bayuquan, Xiaochangshan, and Yantai; with vertical motion rates of-1.82±0.50,-1.65±0.46,-0.88±0.42,-0.58±0.62,-0.13±0.43, and-0.01±0.43 mm/yr, respectively. Upward trends were seen at the three tide gauge stations located at Qinhuangdao, Huludao and Chengshantou; with vertical motion rates of 1.12±0.46, 0.55±0.49 and 0.26±0.44 mm/yr, respectively. There was significant subsidence in Tanggu and Longkou, and a rising trend in Qinhuangdao. According to our results, the rate of sea level rise calculated from these tide gauge records can be improved using a more accurate measurement of the land elevation accounting for lifting or subsidence. The model derived can be used to estimate vertical motions of tide gauge stations, and can be widely applied to revise the benchmark levels of tide gauges. 相似文献
992.
993.
994.
C. Damiani C. Maceroni D. Cardini J. Debosscher L. Balaguer-Núñez I. Ribas 《Astrophysics and Space Science》2010,328(1-2):91-96
We present an on-going study of CoRoT 102931335. Our preliminary results indicate that the target is an eclipsing binary system with an orbital period of $3{.\!\!\vphantom{0}^{\mathrm{d}}}979$ and a primary component pulsating in the frequency range 0.6–0.8 c/d. The results of a ground-based follow-up program provided four-colour Strömgren photometry and allowed us to infer the spectral class and the primary effective temperature. We devised and applied an iterative procedure to disentangle the effects of binarity from those of pulsations and could test that a detailed binary modelling is essential for the purpose. Our results suggest that the pulsating component of CoRoT 102931335 could be a γ Dor variable, a rare occurrence in an eclipsing system. 相似文献
995.
996.
This study examines the time and regime dependencies of sensitive areas identified by the conditional nonlinear optimal perturbation(CNOP) method for forecasts of two typhoons.Typhoon Meari(2004) was weakly nonlinear and is herein referred to as the linear case,while Typhoon Matsa(2005) was strongly nonlinear and is herein referred to as the nonlinear case.In the linear case,the sensitive areas identified for special forecast times when the initial time was fixed resembled those identified for other forecast times.Targeted observations deployed to improve a special time forecast would thus also benefit forecasts at other times.In the nonlinear case,the similarities among the sensitive areas identified for different forecast times were more limited.The deployment of targeted observations in the nonlinear case would therefore need to be adapted to achieve large improvements for different targeted forecasts.For both cases,the closer the forecast time,the higher the similarities of the sensitive areas.When the forecast time was fixed,the sensitive areas in the linear case diverged continuously from the verification area as the forecast period lengthened,while those in the nonlinear case were always located around the initial cyclones.The deployment of targeted observations to improve a special forecast depends strongly on the time of deployment.An examination of the efficiency gained by reducing initial errors within the identified sensitive areas confirmed these results.In general,the greatest improvement in a special time forecast was obtained by identifying the sensitive areas for the corresponding forecast time period. 相似文献
997.
Responses of soil carbon variation to climate variability in China using the LPJ model 总被引:1,自引:1,他引:0
In this study, we explored the maximal response of soil carbon in a part of China to climate change, including variations in climatology and climate variability, under the condition of global warming. A conditional nonlinear optimal perturbation (CNOP) approach was employed to discuss the above issue using the Lund–Potsdam–Jena (LPJ) model. The variation in the soil carbon was compared with those caused by a linear temperature or precipitation perturbation. The key difference between the CNOP-type and the linear perturbations depended on whether the perturbations brought the variation in the temperature or the precipitation variability in comparison with the reference temperature or the precipitation variability. The model results demonstrated that the variations in the soil carbon resulted from the CNOP-type and linear temperature perturbations in south of the study region, which was corresponding to part of South China, had different variations. We examined three components of the soil carbon in the LPJ model: fast-decomposing soil carbon, slow-decomposing soil carbon, and litter below the ground. The variations of these components derived by the two types of temperature perturbations were different in the chosen region. The reduction in the litter below the ground may be the main cause of decreased soil carbon in arid and semi-arid regions as a result of the two types of temperature perturbations. The different impacts of the two types of temperature perturbations in the south of the study region may be mainly caused by the variations in the fast-decomposing soil carbon. The variations in the soil carbon caused by the two types of precipitation perturbations were similar. In the arid and semi-arid regions, the soil carbon increased due to the two types of precipitation perturbations. This research implies that the variation in temperature variability plays a crucial role in the variations of the soil carbon and its components in the study region. 相似文献
998.
A new jadeitite jade locality (Sierra del Convento, Cuba): first report and some petrological and archeological implications 总被引:1,自引:1,他引:0
Antonio García-Casco A. Rodríguez Vega J. Cárdenas Párraga M. A. Iturralde-Vinent C. Lázaro I. Blanco Quintero Y. Rojas Agramonte A. Kröner K. Núñez Cambra G. Millán R. L. Torres-Roldán S. Carrasquilla 《Contributions to Mineralogy and Petrology》2009,158(1):1-16
A new jadeitite jade locality has been discovered in the serpentinite-matrix subduction mélange of the Sierra del Convento
(eastern Cuba) in a context associated with tectonic blocks of garnet-epidote amphibolite, tonalitic–trondhjemitic epidote
gneiss, and blueschist. The mineral assemblages of jadeitite jade and jadeite rocks are varied and include combinations of
jadeite, omphacite, albite, paragonite, analcime, clinozoisite-epidote, apatite, phlogopite, phengite, chlorite, glaucophane,
titanite, rutile, zircon, and quartz formed during various stages in their P–T evolution. Field relationships are obscure,
but some samples made almost exclusively of jadeite show evidence of crystallization from fluid in veins. In one of these
samples studied in detail jadeite shows complex textural and chemical characteristics (including oscillatory zoning) that
denote growth in a changing chemical medium. It is proposed that interaction of an Al–Na rich fluid with ultramafic rocks
produced Al–Na–Mg–Ca fluids of varying composition. Episodic infiltration of these fluids, as a result of episodic opening
of the veins, developed oscillatory zoning by direct precipitation from fluid and after reaction of fluid with pre-existing
jadeite. The latest infiltrating fluids were richer in Mg–Ca, favouring the formation of omphacite and Mg–Ca rich jadeite
in open voids and the replacement of earlier jadeite by fine-grained omphacite + jadeite at 550–560°C. This new occurrence
of jadeite in Cuba opens important perspectives for archeological studies of pre-Columbian jade artifacts in the Caribbean
region. 相似文献
999.
W. A. Ambrose C. Breton M. H. Holtz V. Núñez-López S. D. Hovorka I. J. Duncan 《Environmental Geology》2009,57(7):1537-1551
Documenting geographic distribution and spatial linkages between CO2 sources and potential sinks in areas with significant levels of CO2 emissions is important when considering carbon-management strategies such as geologic sequestration or enhanced oil recovery
(EOR). For example, the US Gulf Coast overlies a thick succession (>6,000 m [>20,000 ft]) of highly porous and permeable sandstone
formations separated by thick, regionally extensive shale aquitards. The Gulf Coast and Permian Basin also have a large potential
for EOR, in which CO2 injected into suitable oil reservoirs could be followed by long-term storage of CO2 in nonproductive formations below reservoir intervals. For example, >6 billion barrels (Bbbl) of oil from 182 large reservoirs
is technically recoverable in the Permian Basin as a result of miscible-CO2 flooding. The Gulf Coast also contains an additional 4.5 Bbbl of oil that could be produced by using miscible CO2. Although the CO2 pipeline infrastructure is well-developed in the Permian Basin, east Texas and the Texas Gulf Coast may have a greater long-term
potential for deep, permanent storage of CO2 because of thick brine-bearing formations near both major subsurface and point sources of CO2. 相似文献
1000.
The impact of disposal and treatment of coal mining wastes on environment and farmland 总被引:9,自引:0,他引:9
Zhengfu Bian Jihong Dong Shaogang Lei Hailong Leng Shouguo Mu Hui Wang 《Environmental Geology》2009,58(3):625-634
In China, coal mining wastes have traditionally been dumped in cone-shaped heaps that have the potential to pollute air, soil
and water environments and landscapes through dust generation, leachate production, self-ignition and as a consequence of
an absence of vegetation cover. Since 1980s, the disposal technique for coal mining wastes has been changing and in many instances
the wastes are now transported directly to subsided land as a fill to enable the reuse of that land. Thus, today, both coal
mining waste dumps from the past and filled subsided lands are in existence. However, the comparative impacts of these different
disposal techniques on the environment and farmland productivity have not been studied in detail. Using Dongtan (DT), Nantun
(NT) and Xinglongzhuang (XLZ) coal mines as examples, the components of coal mining wastes and their potential pollution contribution
to soil, surface water and ground water are tested in-situ. The results show that contaminants are released after self-ignition
and weathering of coal mining wastes, but they are not above the allowable environmental standards. However, despite these
findings, more and closer attention needs to be paid to the mobility, transportation and accumulation of these contaminants
in the environment over time. 相似文献