A mussel and seawater monitoring survey was conducted at six sampling points between Yalikoy (Ordu) and Sinop in 1999-2000 along the Mid-Black Sea Coast of Turkey in order to assess concentrations of organochlorine pesticides (OCs) and polychlorinated biphenyls (PCBs). Chlorinated pesticides and PCBs were measured in the mussel Mytilus Galloprovincialis and in seawater. In the mussel samples, the most common pollutants in terms of average concentration per g of wet weight (ww), were DDT (max. 1800 pg/gww, min. 240 pg/gww) and its metabolites DDD (max. 5400 pg/gww, min. 240 pg/gww) and DDE (max. 2800 pg/gww, min. 70 pg/gww). Also, dieldrin, heptachlor and HCB were notable contaminants in the mussel samples. PCBs were determined in none of the biota or seawater samples. The concentrations of the OCs and PCBs in mussels were higher in coastal areas receiving river discharges and close to the largest city of the region, Samsun (especially in sampling points in the harbour area). The well-known long persistence of DDTs and other chlorinated compounds was confirmed by residues of these pollutants measured in mussels. On the other hand, even though the usage of such kind of persistent compounds in Turkey was banned, there may still be illegal usage and it is not certain whether the application of these compounds did end in the region. 相似文献
Semarang is one of the biggest cities in Indonesia and nowadays suffering from extended land subsidence, which is due to groundwater
withdrawal, to natural consolidation of alluvium soil and to the load of constructions. Land subsidence causes damages to
infrastructure, buildings, and results in tides moving into low-lying areas. Up to the present, there has been no comprehensive
information about the land subsidence and its monitoring in Semarang. This paper examines digital elevation model (DEM) and
benchmark data in Geographic Information System (GIS) raster operation for the monitoring of the land subsidence in Semarang.
This method will predict and quantify the extent of subsidence in future years. The future land subsidence prediction is generated
from the expected future DEM in GIS environment using ILWIS package. The procedure is useful especially in areas with scarce
data. The resulting maps designate the area of land subsidence that increases rapidly and it is predicted that in 2020, an
area of 27.5 ha will be situated 1.5–2.0 m below sea level. This calculation is based on the assumption that the rate of land
subsidence is linear and no action is taken to protect the area from subsidence. 相似文献
One of the specific problems related to historical structures is the fact that they are prone to damage caused by even very
small deformations acting over a long period of time, such as creep or extremely small rock displacements. If any damage has
already occurred, the determination of the rock slope failure mechanism is one of the prerequisites for successful mitigation
technique selection. In this study a medieval castle in central Japan, suffering damage caused by deformation of the rock
mass in the subgrade of the castle, was investigated using a combination of field investigation, high-precision monitoring
and physical modeling experiments. Using these techniques an attempt to determine the failure mechanism of the rock slope
was made. Based on the field investigation a toe-slope failure seemed to be the main triggering factor activating the deformations
in the upper slope area, right below the defense walls of the castle. The displacement monitoring of the surface rock blocks
revealed a slumping failure with the backward rotational component prevailing over the sliding in the immediate vicinity of
the castle wall. This was in accordance with the expectations obtained from the structural analysis of the rock mass carried
out during the field investigation. The displacements obtained during the rock block monitoring, especially from the crack
gauges, were not sufficient for drawing a satisfactory conclusions about the failure mechanism of the blocks located in the
central part of the slope. Therefore, the failure mechanisms of rock blocks inferred from their displacements obtained from
the monitoring were correlated with the results of modeling experiments carried out on the scaled slope model. The physical
modeling revealed a possibility of toppling failure of rock blocks in the central area of the slope caused mainly by block
interlocking, which was supported by the data from surface tilt meters installed additionally in the field. Furthermore, the
possibility of the occurrence of forward and backward rock block rotations in the same sliding body at given conditions was
supported by the physical modeling experiments. 相似文献
We present two case studies regarding the application of Synthetic Aperture Radar (SAR) Persistent Scatterers Interferometry (PSI) techniques to landslide-prone slopes situated in the municipal territories of Caramanico Terme and Volturino (Italy). The analysis of satellite SAR data with PSI techniques poses often problems on sites where, due to the scarcity of human artefacts and the presence of vegetation cover, density of coherent points (PS) is low (< 10 per km2). Moreover, the steep and rough topography typical of landslide-prone areas hamper the interferometric pre-processing, making more difficult the joint estimation of displacements and of DEM errors. Under these conditions the significance of temporal interferometric phase trends can be uncertain and conservative assumptions, necessary to ensure low false detection probabilities, need to be coupled with innovative processing strategies to increase the detection efficiency of PS objects. Here, the SPINUA (Stable Point Interferometry over Un-urbanised Areas) processing technique is applied together with an alternative PS Candidate (PSC) selection procedure based on the use of pixels classified as urban.
The cases of Caramanico and Volturino are representative, respectively, of harsh and favourable conditions for PSI applications. The results from Caramanico show clusters of PS exhibiting similar line-of-sight (LOS) deformation behaviour in the period 1995–2000. The locations of moving PS often coincide with distressed buildings and appear consistent with the areal distribution of recent and past landslide activity. The temporal displacement trends, however, are characterised by very low annual average velocities (from 3 to 7 mm/y) and it is uncertain to what extent the PS data reflect true slope movements, local deformations (e.g. settlement of engineering structures) or both.
Thanks to the more favourable conditions, the application of the standard SPINUA approach in the Volturino area was sufficient to obtain suitable densities of PS, as well as spatially and temporally consistent displacement results for a period 1992–2000. In particular, a group of moving PS was identified in a peri-urban area, known for the past and recent slope stability problems. The slowly moving PS (from 3 to 5 mm/y) fall in a location that, unlike the remaining part of the town, is characterised by the presence of many distressed buildings and structures. Although the site information confirms the reliability of PS data, in the absence of ground monitoring and detailed records of landslide movements, it is difficult to identify the main mechanism of the detected deformations. In general, in geologically and topographically complex urban/peri-urban settings, the significance of very low-velocity PSI surface displacements should always be considered together with in situ geotechnical controls and ground monitoring data. 相似文献
A series of mass wasting events occurred above a Washington, USA, highway in the Cascade Mountains in November and December 2003. The largest event was a rockslide involving approximately 750,000 m3 that occurred on November 9, 2003. The source zone for this event was located at the crest of a ridge. Most of the debris fell to the east of the sharp ridge and was deposited in the relatively shallow sloping Afternoon Creek without causing damage to the highway. Lesser amounts of debris fell to the west of the ridge, sliding 600 m down the steeper Falls Creek and impacting the road. There is an evidence of one or more historical rock avalanches at this location. Displacement of reference points, ground vibration, crack extension, and tilting are being monitored due to concerns that future slope failures or remobilization of debris might again damage or block the highway. 相似文献
During spring 2006, talus from the toe area of a rock-block slide of about 800,000 m3 buried California State Highway 140, one of the main routes into heavily-visited Yosemite National Park, USA. Closure of
the highway for 92 days caused business losses of about 4.8 million USD. The rock slide, composed of slate and phyllite, moved
slowly downslope from April to June 2006, creating a fresh head scarp with 9–12 m of displacement. Movement of the main rock
slide, a re-activation of an older slide, was triggered by an exceptionally wet spring 2006, following a very wet spring 2005.
As of autumn 2006, most of the main slide appeared to be at rest, although rocks occasionally continued to fall from steep,
fractured rock masses at the toe area of the slide. Future behavior of the slide is difficult to predict, but possible scenarios
range from continued scattered rock fall to complete rapid failure of the entire mass. Although unlikely except under very
destabilizing circumstances, a worst-case, rapid failure of the entire rock slide could extend across the Merced River, damming
the river and creating a reservoir. As a temporary measure, traffic has been rerouted to the opposite side of the Merced River
at about the same elevation as the buried section of Highway 140. A state-of-the-art monitoring system has been installed
to detect movement in the steep talus slope, movement of the main slide mass, local strong ground motion from regional earthquakes,
and sudden changes in stream levels, possibly indicating damming of the river by slide material. 相似文献