74 research outputs found

    Rainfall threshold for initiating effective stress decrease and failure in weathered tephra slopes

    Get PDF
    Rainfall is one of the most important triggers of slope failure. Weathered pyroclastic (tephra) deposits are especially vulnerable to slope failure because they commonly form slopes of high porosity and high clay content. Empirically derived thresholds for the triggering of landslides are commonly based on rainfall conditions and have been widely applied in volcanic soils. However, so far only few researchers utilized pore water pressure in the slope as additional variable for the threshold calibration. Here, we derived a new rainfall threshold for initiating the decrease in effective stress in the slope by analyzing a long-term record of rainfall and piezometer data from a slide-prone coastal area in northern New Zealand that consists of clayey, halloysitic tephra deposits. The level of effective stress decrease increased with rainfall intensity and duration. We observed highest effective stress decrease of up to 36% during rainfall events that triggered landslides in our study area. The effective stress threshold exhibits a satisfactory predictive capability. The probability of correctly predicting a decrease in effective stress is 53%. The effective stress threshold contributes towards the implementation of the decrease in effective stress into rainfall thresholds for the occurrence of landslides

    EARLYDRAIN- outcome after early lumbar CSF-drainage in aneurysmal subarachnoid hemorrhage: study protocol for a randomized controlled trial

    Get PDF
    <p>Abstract</p> <p>Background</p> <p>Aneurysmal subarachnoid hemorrhage (SAH) may be complicated by delayed cerebral ischemia, which is a major cause of unfavorable clinical outcome and death in SAH-patients. Delayed cerebral ischemia is presumably related to the development of vasospasm triggered by the presence of blood in the basal cisterns. To date, oral application of the calcium antagonist nimodipine is the only prophylactic treatment for vasospasm recognized under international guidelines.</p> <p>In retrospective trials lumbar drainage of cerebrospinal fluid has been shown to be a safe and feasible measure to remove the blood from the basal cisterns and decrease the incidence of delayed cerebral ischemia and vasospasm in the respective study populations. However, the efficacy of lumbar drainage has not been evaluated prospectively in a randomized controlled trial yet.</p> <p>Methods/Design</p> <p>This is a protocol for a 2-arm randomized controlled trial to compare an intervention group receiving early continuous lumbar CSF-drainage and standard neurointensive care to a control group receiving standard neurointensive care only. Adults suffering from a first aneurysmal subarachnoid hemorrhage whose aneurysm has been secured by means of coiling or clipping are eligible for trial participation. The effect of early CSF drainage (starting < 72 h after securing the aneurysm) will be measured in the following ways: the primary endpoint will be disability after 6 months, assessed by a blinded investigator during a personal visit or standardized telephone interview using the modified Rankin Scale. Secondary endpoints include mortality after 6 months, angiographic vasospasm, transcranial Doppler sonography (TCD) mean flow velocity in both middle cerebral arteries and rate of shunt insertion at 6 months after hospital discharge.</p> <p>Discussion</p> <p>Here, we present the study design of a multicenter prospective randomized controlled trial to investigate whether early application of a lumbar drainage improves clinical outcome after aneurysmal subarachnoid hemorrhage.</p> <p>Trial registration</p> <p>www.clinicaltrials.gov Identifier: <a href="http://www.clinicaltrials.gov/ct2/show/NCT01258257">NCT01258257</a></p

    A new attraction-detachment model for explaining flow sliding in clay-rich tephras

    Get PDF
    Altered pyroclastic (tephra) deposits are highly susceptible to landsliding, leading to fatalities and property damage every year. Halloysite, a low-activity clay mineral, is commonly associated with landslide-prone layers within altered tephra successions, especially in deposits with high sensitivity, which describes the post-failure strength loss. However, the precise role of halloysite in the development of sensitivity, and thus in sudden and unpredictable landsliding, is unknown. Here we show that an abundance of mushroom cap–shaped (MCS) spheroidal halloysite governs the development of sensitivity, and hence proneness to landsliding, in altered rhyolitic tephras, North Island, New Zealand. We found that a highly sensitive layer, which was involved in a flow slide, has a remarkably high content of aggregated MCS spheroids with substantial openings on one side. We suggest that short-range electrostatic and van der Waals interactions enabled the MCS spheroids to form interconnected aggregates by attraction between the edges of numerous paired silanol and aluminol sheets that are exposed in the openings and the convex silanol faces on the exterior surfaces of adjacent MCS spheroids. If these weak attractions are overcome during slope failure, multiple, weakly attracted MCS spheroids can be separated from one another, and the prevailing repulsion between exterior MCS surfaces results in a low remolded shear strength, a high sensitivity, and a high propensity for flow sliding. The evidence indicates that the attraction-detachment model explains the high sensitivity and contributes to an improved understanding of the mechanisms of flow sliding in sensitive, altered tephras rich in spheroidal halloysite

    Mobile Air Quality Studies (MAQS) - an international project

    Get PDF
    Due to an increasing awareness of the potential hazardousness of air pollutants, new laws, rules and guidelines have recently been implemented globally. In this respect, numerous studies have addressed traffic-related exposure to particulate matter using stationary technology so far. By contrast, only few studies used the advanced technology of mobile exposure analysis. The Mobile Air Quality Study (MAQS) addresses the issue of air pollutant exposure by combining advanced high-granularity spatial-temporal analysis with vehicle-mounted, person-mounted and roadside sensors. The MAQS-platform will be used by international collaborators in order 1) to assess air pollutant exposure in relation to road structure, 2) to assess air pollutant exposure in relation to traffic density, 3) to assess air pollutant exposure in relation to weather conditions, 4) to compare exposure within vehicles between front and back seat (children) positions, and 5) to evaluate "traffic zone"- exposure in relation to non-"traffic zone"-exposure. Primarily, the MAQS-platform will focus on particulate matter. With the establishment of advanced mobile analysis tools, it is planed to extend the analysis to other pollutants including including NO2, SO2, nanoparticles, and ozone

    The mechanical behavior of gas hydrate in the pore space of marine sediments modeled with the Distinct Element Method.

    No full text
    The mechanical behavior of gas hydrate bearing sediment is a possible trigger for huge tsunami generating slides on continental margins, but little is known of gas hydrates mechanical behavior in sediment. Here a method is proposed to simulate the behavior of gas hydrate in sediment on the pore scale using the Distinct Element Method (DEM). The simulation is founded on the surface energy, which is the cause for the forces exerted by growing crystals. The simulation uses attractive particle interaction and random particle agitation to generate a surface tensed material. The method is calibrated and validated by a series of different experiments. Gas hydrate growth is simulated in an oedometer. The influence of the host sediment fabric on gas hydrate fabric is investigated in a series of element tests and compared to natural gas hydrate fabrics

    Modellierung von Gashydraten und deren Wachstumsverhalten im Porenraum mariner Sedimente mit Hilfe der Distinkte Elemente Methode.

    No full text
    The mechanical behavior of gas hydrate bearing sediment is a possible trigger for huge tsunami generating slides on continental margins, but little is known of gas hydrates mechanical behavior in sediment. Here a method is proposed to simulate the behavior of gas hydrate in sediment on the pore scale using the Distinct Element Method (DEM). The simulation is founded on the surface energy, which is the cause for the forces exerted by growing crystals. The simulation uses attractive particle interaction and random particle agitation to generate a surface tensed material. The method is calibrated and validated by a series of different experiments. Gas hydrate growth is simulated in an oedometer. The influence of the host sediment fabric on gas hydrate fabric is investigated in a series of element tests and compared to natural gas hydrate fabrics

    CPT datasets showing the effect of horizontal spacing on cone resistance for sand deposit in Bremen, Germany

    No full text
    Geotechnical methods, such as cone penetration tests (CPT), standard penetration tests (SPT), and seismic cone penetration tests (sCPT), are widely used to characterize the in-situ properties of soil. In studies where more than one in situ method in close spacing is used, it is important for geotechnical engineers to balance between soil heterogeneity and the artefacts of disturbed testing zones. The same applies if a detailed information about the subsoil is required and one in situ method is used in close spacing. There is no consensus on how to define the minimum spacing between testing zones and no study on the effect of disturbance caused by in situ tests. In this study, 33 CPTs were performed in natural sediments in Northern Germany and spacing threshold was defined at which cone resistance is affected by soil disturbance from previously performed CPTs. The CPTs were performed sequentially by successively refining the grid spacing, starting with a spacing of 119 cone diameters between CPTs, to a fine grid spacing of 7 cone diameters. The cone resistance is affected by previous CPT measurements below a spacing threshold of 24 cone diameters in medium-dense sands. Silt and clay layers showed no reduction in the cone resistance for the minimum grid spacing of 7 cone diameters
    • 

    corecore