Isotopic composition of Late Mesozoic basic and ultrabasic rocks from the Andes (23–32°S) – implications for the Andean mantle     

Friedrich Lucassen  Monica Escayola  Rolf L. Romer  José Viramonte  Kerstin Koch  Gerhard Franz 《Contributions to Mineralogy and Petrology》2002,143(3):336-349

  相似文献   

Desertification in reverse? Observations from northern Burkina Faso   总被引：1，自引：0，他引：1  

Kjeld Rasmussen  Bjarne Fog  Jens E. Madsen 《Global Environmental Change》2001,11(4):1707

The idea of degradation of arid and semi-arid lands, often termed desertification in its irreversible form, due to human impact and/or climatic change has been much debated since the mid-1970s. From the time of the United Nation's Conference On Desertification in Nairobi, 1976, certain areas of northern Burkina Faso have been pointed out as examples of severe desertification. Several studies demonstrated that revitalization of a series of E–W oriented fossille dunes in the Oudalan province was ongoing. The present study includes an analysis of the trends of vegetation development in the region, covering the period 1955 to 1994, with emphasis on the fossile dunes. It is demonstrated that desertification and revitalization of dunes were phenomena associated with the period between the early 1970s and the mid-1980s, and that the decline in vegetation cover on the dunes seems to have been reversed in recent years. The analysis is based upon time series of aerial photos and satellite images, field studies of vegetation, interviews with local people and review of relevant literature. The findings are discussed with reference to the debate concerning desertification and land degradation, as well as to the current revisions of the ‘range management paradigm’. The observations indicate that the environmental history of the region is complex and cannot be boiled down to ‘human-induced irreversible degradation’. Rather they support the idea of semi-arid cultural landscapes undergoing constant change in response to both human impact and climatic trends and fluctuations.  相似文献   

Regulation of Injected Ground Water Tracers   总被引：1，自引：0，他引：1  

Skelly A. Holmbeck-Pelham  Todd C. Rasmussen  Laurie A. Fowler 《Ground water》2000,38(4):541-549

  相似文献   

Geochemistry of salt marsh sediments deposited during simulated sea-level rise and consequences for recent and Holocene coastal development of NW Germany   总被引：2，自引：2，他引：0  

Kerstin Kolditz  Olaf Dellwig  Jan Barkowski  Thomas H. Badewien  Holger Freund  Hans-Jürgen Brumsack 《Geo-Marine Letters》2012,32(1):49-60

De-embankment in the salt marshes of the island of Langeoog was carried out in 2004, thereby inducing an artificial transgression within an area of 2.2 km². Material from three suspended matter traps (SMTs) located along a N–S transect was collected monthly between January 2006 and February 2007. Besides geochemical (major and trace elements) and grain-size analyses, the duration and height of water cover were continuously measured by pressure gauges during the sampling period at two sites, thus revealing inundation frequency (max. 280 year⁻¹) and level (max. 2.4 m). Generally, the silt-dominated SMT material exhibits a geochemical composition similar to that of suspended particulate matter from the adjacent Wadden Sea. However, distinctly increasing enrichments of TOC, P, Mn and Mo from the shoreline towards the higher salt marsh clearly indicate fractionation processes during material transport. Geochemical comparison with older Holocene coastal deposits reveals a mixture of brackish and tidal flat sediments, thus reflecting an early stage of sea-level rise and the development from a terrestrial towards a marine-dominated system. Sedimentation rates are higher than the local sea-level rise, as revealed by vertical salt marsh growth. Storm surges deliver the highest amounts of sediment and play an important role in salt marsh accumulation within the study area. Average accumulation rates of TOC (780 t year⁻¹), P (54 t year⁻¹) and Mn (5.2 t year⁻¹) in the de-embanked area suggest that the former sand-dominated sediments currently receive significant amounts of reactive organic-rich material, thus fostering biogeochemical cycling.  相似文献   

Sustainable land use in Tikopia: Food production and consumption in an isolated agricultural system   总被引：3，自引：3，他引：0  

Ole Mertz  Thilde Bech Bruun  Bjarne Fog  Kjeld Rasmussen  Jytte Agergaard 《Singapore journal of tropical geography》2010,31(1):10-26

The land use system on Tikopia – a Polynesian outlier in Solomon Islands – is analyzed to determine how it has developed since it was first described in the 1930s and again in the 1970s. Fieldwork included a household questionnaire survey, in-depth interviews on farming practices and decision making, and the collection of soil samples from the major soil and garden types. The Tikopian land use system has not undergone significant changes since the 1970s; indeed the focus on self-sufficiency in food crops may have been strengthened over the past 30 years as ship arrivals have become increasingly unreliable. Local agricultural production and exploitation of marine resources are essential to sustain the population, and with few exceptions farming and fishing techniques remain unchanged. Most of the island is still farmed permanently and the intensive agricultural system has not suffered long-term setbacks, not even from extreme events such as Cyclone Zoe in 2002. The high fertility of Tikopian soils reported in the 1960s was found to be unchanged. It is concluded that the land use system is highly resilient to shocks and that there are no indications that Tikopian villagers would not be able to support their subsistence in the future, provided there is no substantial increase in the resident ( de facto ) population.  相似文献   

Sensitivity of freezing drizzle formation in stably stratified clouds to ice processes   总被引：1，自引：0，他引：1  

I. Geresdi  R. Rasmussen  W. Grabowski  B. Bernstein 《Meteorology and Atmospheric Physics》2005,88(1-2):91-105

Summary This study examines the impact of ice formation and growth processes on freezing drizzle formation in stably stratified clouds. In particular we investigate the reason why freezing drizzle is rarely observed in clouds with top temperatures less than –15°C. We also investigate the sensitivity of freezing drizzle formation to the Hallett Mossop secondary ice process (Hallet and Mossop, 1974). The evaluation is performed by simulating cloud formation over a two-dimensional idealized mountain using a detailed microphysical scheme. The height and width of the two-dimensional mountain were designed to produce an updraft pattern with extent and magnitude similar to documented freezing drizzle cases. The simulations show that: (i) drizzle formation is very sensitive to the ice crystal concentration, with a significant reduction in the area over which drizzle forms and the maximum drizzle water content as the cloud top temperature decreases below –10°C, and (ii) secondary ice crystal formation has a significant effect on drizzle formation at cloud top temperatures below –10°C.The above two factors are likely the main cause for the lack of freezing drizzle at cloud top temperatures less than –15°C. We also found that neglecting the depletion of ice forming nuclei resulted in considerable overestimation of the ice crystal concentration and suppression of drizzle, even for the –10°C case.  相似文献   

Trace Element Partitioning between Taenite and Kamacite; Relationship to the Cooling Rates of Iron Meteorites     

Kaare L. Rasmussen  Daniel J. Malvin  John T. Wasson 《Meteoritics & planetary science》1988,23(2):107-112

Abstract— Instrumental neutron activation analysis (INAA) was used to determine Ni, Co, Cu, Ga, As, Au, W, Re and Ir in taenite lamellae isolated by acid dissolution from eight iron meteorites from groups IA, IIIAB and IVA. Taenite is enriched in Ni, Cu, Ga, As, Au, W, Re and Ir relative to kamacite, whereas taenite is depleted in Co. Taenite/kamacite partition ratios in slowly cooled IAB meteorites are farther from unity than those in rapidly cooled IVA meteorites. Taenite/kamacite partition ratios for Cu, Ir, Au and Co may be sensitive cooling rate indicators.  相似文献   

Magnetotellurics along the Fennoscandian Long Range profile   总被引：2，自引：0，他引：2  

T. M. Rasmussen  R. G. Roberts  L. B. Pedersen 《Geophysical Journal International》1987,89(3):799-820

Summary. Estimates of magnetotelluric transfer functions along the Fennoscandian Long Range (FENNOLORA) profile are presented and discussed in relation to the major lithotectonic subdivisions of the Swedish part of the Baltic shield. None of the transfer functions are found to be consistent with a one-dimensional earth structure, thereby making a quantitative interpretation difficult. However, the geological units are found to display characteristic differences in the obtained transfer functions, and in some areas a quantitative interpretation can be justified. The most interesting structure indicated is a low resistive (4 μm) crustal structure of lateral extension more than 150 km centred around the Skellefte ore district. A minimum thickness for this structure of 15 km is inferred.  相似文献   

Paleolimnology of three Jackman Sound Lakes,Southern Baffin Island,based on down-core diatom analyses     

Kerstin M. Williams 《Journal of Paleolimnology》1990,4(3):203-217

Three lakes, informally named Lakes Inqua, Instaar and Mercer, from the Jackman Sound area in Southern Baffin Island were cored. The elevation of the three lakes are 36 m above high tide (aht), 10 m aht and 1 m aht. The cores from Lakes Inqua and Mercer penetrated the marine/lacustrine boundary; the core from Lake Instaar is estimated to have come within ca. 5 cm of this boundary. In addition, grab samples and water samples were retrieved from the lakes. The cores have been ¹⁴C dated (AMS). Emergence of the three lake basins from the sea occurred approximately 8650 BP (Lake Inqua), 8630 BP (Lake Instaar) and 7900 BP (Lake Mercer, averaged date). This suggests a very rapid rate (>5 m/100 yrs) of glacio-isostatic rebound for this area. Down-core analyses of diatom assemblages indicate that the paleolimnology in the three lakes was similar. The diatom analyses suggest a change in climate between approximately 8000 and 6000 BP, which is also reflected in the marine record from the same area, and the onset of the neoglacial period around 4500 to 3800 BP. A decrease in diatom-inferred pH is evident in the lakes' development and can probably be related to the general change of the watershed vegetation with time.  相似文献   

Historical ecology of a central California estuary: 150 years of habitat change   总被引：1，自引：0，他引：1  

Eric Van Dyke  Kerstin Wasson 《Estuaries and Coasts》2005,28(2):173-189

We investigated the historical ecology of Elkhorn Slough, a 1,200 ha tidal wetland system in central California. The goal of this study was to identify patterns of change in the extent and distribution of wetland habitats during a 150-yr period and to investigate the causes of these changes. Using a geographic information system (GIS), we interpreted historic maps, charts, and aerial photographs. We created a series of summary maps to illustrate and quantify changes in tidal flow and habitat types at six representative historical periods. With the aid of custom software tools, we performed semi-automated spatial analysis of historic aerial photographs to quantify changes in marsh cover at fixed quadrats and tidal creek width at fixed cross sections. Our multiscale analysis documents dramatic shifts in the distribution of habitat types resulting from anthropogenic modifications to the hydrology of the slough. More than half of the marshlands were diked, and more than two thirds have either degraded or been converted to other habitat types. The construction of an artificial mouth abruptly transformed the wetland system from depositional to highly erosional, enlarging channels, widening creeks, and converting marsh to intertidal mudflat or open water. Increased tidal amplitude and velocity are the likely causes. In recent decades, levee failure and intentional breaching have restored the acreage under tidal influence to nearly historic levels, but recolonization of former wetlands by salt marsh vegetation has been minimal. Degraded former marshland and unvegetated mudflat are now the dominant habitat types at Elkhorn Slough. The rate of habitat change remains high, suggesting that a new equilibrium may not be reached for many decades. This study can help tidal wetland managers identify patterns and mechanisms of habitat change and set appropriate conservation and restoration goals.  相似文献