Source of error and uncertainty in sheet erosion rates estimated from dendrogeomorphology          下载免费PDF全文

José M. Bodoque  Juan A. Ballesteros‐Cánovas  Ana Lucía  Andrés Díez‐Herrero  José F. Martín‐Duque 《地球表面变化过程与地形》2015,40(9):1146-1157

Dendrogeomorphology has been used since the 1960s to estimate sheet erosion rates. To date, most efforts have focused on accurately determining the first year of root exposure. However, an adequate methodological approach that takes into consideration the microtopography of the ground surface when estimating sheet erosion rates using dendrogeomorphology has not been proposed. In this study, terrestrial laser scanning (TLS) was used for the first time to examine how changes in microtopography determine the level of certainty in estimates. To this end, highly accurate TLS‐based digital elevation models representing exposed roots and their immediate vicinity were analysed using geographic information system tools. The results indicate that erosion rates calculated using the standard dendrogeomorphic method have been underestimated by up to 29% because the method does not take into account changes to the microtopography caused by the axial and radial pressure of the roots. Another source of uncertainty, which we estimate to be 50%, was also found and is the result of changes in the ground surface microtopography caused by variations in soil roughness. These findings do not invalidate the usefulness of dendrogeomorphology for assessing soil erosion, although they do show the need for correct characterization of the microtopography to guarantee reliability. Copyright © 2015 John Wiley & Sons, Ltd.  相似文献   

Sustainable groundwater extraction in coastal areas: a Belgian example   总被引：1，自引：0，他引：1  

Alexander Vandenbohede  Emmanuel Van Houtte  Luc Lebbe 《Environmental Geology》2009,57(4):735-747

Water extractions in coastal areas have to deal with salt water intrusion and lowering of hydraulic heads in valuable ecosystems. Therefore, sustainable management of fresh water resources in these areas is crucial. This is illustrated here with two water extractions in the western Belgian coastal plain which extract groundwater from a phreatic dune aquifer. One water extraction faced problems with salt water intrusion, while lowering of hydraulic heads was an issue for both. To remedy the salt water intrusion, it was found that decreasing the extraction rate was the only solution. To offset this and to increase hydraulic heads around both extractions, it was decided to artificially recharge the aquifer of the second extraction with tertiary treated wastewater. By taking these interventions, the combined production capacity of the water extractions was increased with 56% whereas 27% less water was extracted from the dune aquifer itself. Extraction history and the effects of interventions are illustrated for both water extractions with water quality data and fresh water head observations. A more detailed insight in groundwater flow and fresh–salt water distribution in the aquifer is provided by simulating the evolution of the water extractions with a 3D density dependent groundwater flow model.  相似文献   

Effects of sorption competition on caesium diffusion through compacted argillaceous rock     

Andreas Jakob  Wilfried Pfingsten  Luc Van Loon 《Geochimica et cosmochimica acta》2009,73(9):2441-2456

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Combining two seismic experiments to attenuate free-surface multiples in OBC data*     

Luc T. Ikelle 《Geophysical Prospecting》1999,47(2):179-193

The current inverse scattering solution used for multiple attenuation of marine seismic reflection data assumes that sources and receivers are located in the water. To adapt this solution to the ocean-bottom cable (OBC) experiment where receivers are located on the sea-floor, we have proposed combining the conventional marine surface seismic reflection data (streamer data) with OBC data. The streamer data add to the OBC data some of the wave paths needed for multiple attenuation. This combination has allowed us to develop a multiple attenuation method for OBC data which does not require any knowledge of the subsurface and which takes into account all free-surface multiples, including receiver ghosts. A non-linear synthetic data example consisting of pressure and particle velocity fields is used to illustrate the procedure.  相似文献   

A gamma‐ray spectroscopy survey of Omani meteorites          下载免费PDF全文

Patrick Weber  Beda A. Hofmann  Tamer Tolba  Jean‐Luc Vuilleumier 《Meteoritics & planetary science》2017,52(6):1017-1029

The gamma‐ray activities of 33 meteorite samples (30 ordinary chondrites, 1 Mars meteorite, 1 iron, 1 howardite) collected during Omani‐Swiss meteorite search campaigns 2001–2008 were nondestructively measured using an ultralow background gamma‐ray detector. The results provide several types of information: Potassium and thorium concentrations were found to range within typical values for the meteorite types. Similar mean ²⁶Al activities in groups of ordinary chondrites with (1) weathering degrees W0‐1 and low ¹⁴C terrestrial age and (2) weathering degree W3‐4 and high ¹⁴C terrestrial age are mostly consistent with activities observed in recent falls. The older group shows no significant depletion in ²⁶Al. Among the least weathered samples, one meteorite (SaU 424) was found to contain detectable ²²Na identifying it as a recent fall close to the year 2000. Based on an estimate of the surface area searched, the corresponding fall rate is ~120 events/10⁶ km²*a, consistent with other estimations. Twelve samples from the large JaH 091 strewn field (total mass ~4.5 t) show significant variations of ²⁶Al activities, including the highest values measured, consistent with a meteoroid radius of ~115 cm. Activities of ²³⁸U daughter elements demonstrate terrestrial contamination with ²²⁶Ra and possible loss of ²²²Rn. Recent contamination with small amounts of ¹³⁷Cs is ubiquitous. We conclude that gamma‐ray spectroscopy of a selection of meteorites with low degrees of weathering is particularly useful to detect recent falls among meteorites collected in hot deserts.  相似文献   

A description of internal erosion by suffusion and induced settlements on cohesionless granular matter   总被引：1，自引：1，他引：0  

Luc Sibille  Didier Marot  Yacine Sail 《Acta Geotechnica》2015,10(6):735-748

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Book reviews     

L. Denis Delorme  Luc De Meester  Henri J. Dumont  H. E. Wright Jr. 《Journal of Paleolimnology》1990,3(1):75-79

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ISO SWS Spectroscopy of WR 146 (WC6+O)     

A.J. Willis  Luc Dessart  P.A. Crowther  P.W. Morris  K.A. Van Der Hucht 《Astrophysics and Space Science》1997,255(1-2):167-168

We have obtained ISO SWS spectroscopy of WR 146 (WC6+O) covering the wavelength range 2.6-20 μm. WC6 wind emission is observed in numerous lines of He II and C IV, as well as in the [Ne III] 15.5 μm line, but not in [Ne II] 12.81 or [Ne V] 14.32 μm. An analysis of these spectra (and complementary radio and optical data) yields for the WC6 star: v∞ = 2700 km s-1; M=2.6×10-5M⊙yr-1; C/He = 0.15; and a neon abundance bound of 3.4×10-3≤Ne/He≤6.8×10-3. The neon abundance is close to that predicted in stellar evolution models of WC stars. This revised version was published online in August 2006 with corrections to the Cover Date.  相似文献   

Opaline concretions in Weichselian Late-glacial lake marl from Flanders, northern Belgium     

Luc Denys  Patrick Kiden  Cyriel Verbruggen 《Journal of Paleolimnology》1998,20(1):91-98

Macroscopic opal-A concretions were observed in lake marl deposited in a small Flemish lake (Belgium) during the Allerød biozone of the Weichselian Late-glacial (ca. 12–11 ka BP). The silica from these concretions was derived within the profile, by the leaching of siliceous microfossils – mainly diatom frustules. Formation of the concretions probably resulted from pH- and/or evaporation related precipitation of the silica at a lower stratigraphic level, presumably corresponding more or less to a former low position of the groundwater table. The presence of these concretions is probably related to alternatingly wet and dry local conditions during the middle and later part of the Allerød.  相似文献   

Ionizing Power of Massive Stars in the Cores of Two Giant HII Regions: R136A and HD 97950     

Luc Dessart  Paul Crowther 《Astrophysics and Space Science》1998,260(1-2):177-180

We evaluate the integrated ionizing fluxes in cores of giant HII regions below the important continuum edges, considering both O and WR stars. We find that they contribute in equivalent proportions to the HI and HeI continua, but that only the hottest O stars emit in the HeH continuum. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献