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981.
Karol Kuliński Joanna Święta-Musznicka Andrzej Staniszewski Janusz Pempkowiak Małgorzata Latałowa 《Journal of Paleolimnology》2007,38(4):555-567
The quantity and quality of lignin phenols (Σ8, Λ, S/V, C/V and (Ad/Al)v) in the sediments of three small Lobelia lakes with neither inlets nor outlets were investigated and compared with palynological data and lithology of the profiles.
The method of alkaline CuO oxidation was used. Substantial differences with respect to sedimentary lignin concentration and
provenance recorded along the profiles and among the sites are in good agreement with pollen data describing the dominant
type of vegetation and with indices of soil erosion in the lakes’ catchments. This relation shows that the compositions of
lignin degradation products in these lakes are closely related to the local environmental conditions. In all the lakes gymnosperm
wood is the main source of lignin products; however, each lake is characterized by different S/V index values. Especially
good correlations were obtained between pine pollen proportions in sediments and the S/V index. The correlation between the
C/V and (Ad/Al)v indices indicates a higher degradation of organic matter when non-woody tissue is more abundant. This pilot study illustrates
the usefulness and potential for a wider application of lignin oxidation products in palaeoecological reconstructions. This
kind of data would be of special importance when investigating local presence/absence of woody plants and the role of angiosperms/gymnosperms
in local vegetation. Estimates of lignin biodegradation levels, as well as the data on diagenetic processes, may afford supplementary
information on possible disturbances in sedimentation. 相似文献
982.
Agnieszka Gałuszka 《Environmental Geology》2007,52(5):861-870
One of the most crucial issues of recent environmental sciences is the topic of background concentrations of elements and
organic compounds in various abiotic and biotic systems. The relationship between natural and anthropogenically altered concentrations
of chemical species is a question that involves many implications in the geosciences, environmental and biological sciences,
toxicology, and other related disciplines. This is especially important when interpreting geochemical and biogeochemical anomalies
of toxic elements and/or organic compounds in various media. To better understand the potential impact of hazardous substances
in the environment, we must become more familiar with their spatial and temporal distribution and with their behavior under
different physico-chemical and biotic conditions. This review presents an assessment of the geochemical background concept
as used by various authors. Different assumptions and approaches to this topic are presented, including direct, statistical,
and integrated methods. Based on the results derived from geochemical and biogeochemical studies performed in selected forest
ecosystems of Poland, an integrated method is presented. As a consequence of data processing, a normal distribution of data
points was obtained using an iterative 2σ-technique. This method of estimating geochemical background is feasible and can
be used for setting environmental quality standards or for studying the impact of anthropogenic pollution sources on the environment. 相似文献
983.
984.
Sławomir Jerzy Gibowicz 《Acta Geophysica》2006,54(2):142-157
The following criteria for selection of doublets at Polish coal mines were accepted: the difference in magnitude (based on
seismic moment) of two events not larger than 0.15, the distance between their hypocenters not greater than 150 m, and the
time interval between their occurrence not longer than 10 days. Similarly, the criteria for seismic events at copper mines
are: the difference in magnitude not exceeding 0.15, the distance not greater than 200 m, and the time interval not longer
than 20 days. Seismic events from the Wujek and Ziemowit coal mines that occurred between 1993 and 1995, and seismic events
from the Polkowice copper mine that occurred between 1994 and 1996 and from the Rudna copper mine that occurred between 1994
and 2004 were considered. Their source parameters and focal mechanisms were known in most cases from previous studies. Altogether
108 seismic pairs from coal mines and 118 pairs from copper mines were found, forming doublets, triplets and quadruplets,
within the magnitude range from 0.7 to 3.5. The distance and time intervals between two events forming pairs are not dependent
on magnitude of these events.
The focal mechanism of seismic events forming pairs is similar in over 60 percent of pairs at coal mines and in about one
third of pairs at copper mines. Spatial distributions of doublets in particular sections of coal and copper mines display
dominant linear trends, characteristic for a given area, which are often in conformity with the direction of nodal planes
determined by fault plane solution of one or both the events forming a doublet. In such cases, the rupture plane can be discriminated
among the nodal planes. 相似文献
985.
Middle-Upper Jurassic carbonates exposed in 7 separate fragments of three tectonic units were sampled in the Polish segment
of the Pieniny Klippen Belt in 1981, before construction of the Niedzica-Czorsztyn dam. Demagnetization experiments performed
about 20 years ago and analyzed lately with modern program package revealed the presence of Middle Miocene overprints acquired
in the normal and reversed geomagnetic field, and pre-folding components of natural remanence acquired during the Middle-Upper
Jurassic. A paleolatitude of 36N±7° was obtained for the studied area for this time on the basis of 3 normal and 1 reversed
components. Three pre-folding pole positions are situated between pole positions of the normal and reversed Stable European
Middle Jurassic field. The obtained paleomagnetic results imply several prefolding (pre-Upper Miocene) and postfolding (post-Upper
Miocene) episodes of rotations of the studied fragments. 相似文献
986.
The paper presents a method for correction of amplitude of prestack migration using the reflectivity function. The solution
of wave equations for heterogeneous media expressed in the form of Neumann series for converted waves was used to find the
reflectivity function. The performance of the proposed method was verified using synthetic models of wavefields. The synthetic
models of wavefields were also used to compare amplitude correction levels required by the presented method and the standard
amplitude correction methods, i.e., the methods using the spherical divergence and extention factor. 相似文献
987.
988.
989.
防震减灾行政行为有关问题概述 总被引:2,自引:2,他引:2
运用行政法学基本原理,结合防震减灾法律、法规和工作实际,初步分析探讨了防震减灾具体行政行为、抽象行政行为的现状及其应有的发展态势。 相似文献
990.
Ana María Sato Hugo Tickyj Eduardo Jorge Llambías Miguel Angelo Stipp Basei Pablo Diego Gonzlez 《Gondwana Research》2004,7(4):1077-1087
The Las Matras Block in Central Argentina constitutes the southernmost part of the Cuyania terrane, which was accreted to the southwestern margin of Gondwana during the Early to Mid Ordovician Famatinian orogeny. The Grenville-aged rocks of the Las Matras Block are represented by the tonalitic to trondhjemitic Las Matras pluton. A new U-Pb conventional zircon age of 1244±42 Ma confirms previous Sm-Nd and Rb-Sr isochron ages of this pluton. Mineral composition data are consistent with the tonalitic-trondhjemitic character of the pluton, and constrain its emplacement level to 1.9 to 2.6 kb. This shallow level of emplacement and the undeformed character of the pluton are distinctive features of this southernmost basement. A regional comparison indicates that the igneous-metamorphic evolution of the Grenville-aged basement rocks of the Cuyania terrane occurred over a period of more than 200 million years, with ages older than 1200 Ma up to those close to 1000 Ma. The shallowest crustal level is found in Las Matras, suggesting a southward shallowing of the exposed level of basement. The deformation and metamorphism associated with the collisional Famatinian orogeny affect both the Cuyania terrane and the adjacent western margin of Gondwana, and the Gondwana margin was also the locus of the related arc magmatism, but the compressive effects of the collision decrease in intensity toward the south. The Famatinian metamorphism and magmatism continue even further south into the Patagonia region, but the southern continuity of the Cuyania terrane into this region remains uncertain. 相似文献