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41.
The geology, hydrology and types of groundwater exploitation of the Amsterdam dune-water catchment area with artificial recharge of water from the river Rhine are briefly introduced. A classification of natural and artificial watertypes in the catchment is presented together with their genesis and distribution in space and time. The natural, vertical, hydrochemical zonation in fresh, brackish and salt groundwaters has been disturbed by decades of overdraft and the subsequent start of artificial recharge since 1957. Various mixed-water types resulted. A detailed case study of a part of the catchment area (around the Barnaart-Schuster Canal) covers a period of about 50 years. The decisive influence of geological inhomogeneities on the patterns of saltwater encroachment during the period of overdraft and on the patterns of infiltration of river water into the deep aquifer after the start of artificial recharge are demonstrated. The shifts in the subsurface positions of the various water types due to changes in the groundwater management of the catchment area are elucidated. They give an example of displacement and dispersion phenomena under field conditions. 相似文献
42.
43.
A simple model for potential dewfall in an arid region 总被引:4,自引:0,他引:4
It is not always easy to know, post-facto, whether both dewfall and fog may have occurred over a given evening period. Instrumentation limitations make it difficult to quantify dew deposition since they rely on artificial sensing surfaces that are either visually examined on a daily basis or recorded. In arid to Mediterranean regions, both dew and fog can play significant ecological roles as suppliers of moisture. Long-term observation records of dew and fog in such regions tend to be limited, however, due partly to a lack of interest and limited distribution of well-instrumented meteorological stations. Simple meteorological criteria are suggested here to calculate potential dewfall and to indicate whether fog was likely to have occurred over a given evening. A field campaign was carried out in the NW Negev desert, Israel, in September and October 1997, to collect meteorological data and carry out dewfall measurements. 相似文献
44.
Anne S. Marsh Daniel P. Rasse Bert G. Drake J. Patrick Megonigal 《Estuaries and Coasts》2005,28(5):694-704
The effects of long-term exposure to elevated atmospheric CO2 (ambient + 340 ppmv) on carbon cycling were investigated for two plant communities in a Chesapeake Bay brackish marsh, one
dominated by the C3 sedgeSchoenplectus americanus and the other by the C4 grassSpartina patens. Elevated CO2 resulted in a significant increase in porewater concentrations of DIC at 30 cm depth (p < 0.1). The CO2 treatment also yielded increases in DOC (15 to 27%) and dissolved CH4 (12–18%) in the C3 marsh (means for several depths over the period of June 1998 and June 1999), but not at a significant level. Elevated CO2 increased mean ecosystem emissions of CO2 (34–393 g C m−2 yr−1) and CH4 (0.21–0.40 g C m−2 yr−1) in the C3 community, but the effects were only significant on certain dates. For example, CO2 enrichment increased C export to the atmosphere in the C3 community during one of two winter seasons measured (p = 0.09). In the C4 community, gross photosynthesis responded relatively weakly to elevated CO2 (18% increase, p > 0.1), and the concomitant effects on dissolved carbon concentrations, respiration, and CH4 emissions were small or absent. We concluded that elevated CO2 has the potential to increase dissolved inorganic carbon export to estuaries. 相似文献
45.
G.B. Engelen 《Journal of Hydrology》1973,18(1):55-79
Recent observations of badland slopes in South Dakota before, during and after a rainstorm revealed the temporary existence of a dense, integrated drainage network of micro-rills, which was completely obliterated by dessication cracks within a few hours after the end of the rains. These additional observations were combined with data from previous studies by Schumm (1956a, 1962) and Smith (1958) to describe in a comprehensive framework the processes of runoff on these slopes and the related micro-morphological forms. 相似文献
46.
There is great international concern over the increase of atmospheric carbon dioxide and its effect on vegetation and climate,
and vice versa. Many studies on this issue are based on climate model calculations or indirect satellite observations. In
contrast we present a 12-year study (1994–2005) on the net ecosystem exchange of carbon dioxide (NEE) and precipitation surplus (i.e., precipitation–evaporation) of a grassland area in the centre of the Netherlands. On basis
of direct flux observations and a process-based model we study and quantify the carbon uptake via assimilation and carbon
release via soil and plant respiration. It appears that nearly year-round the assimilation term dominates, which indicates
an accumulation of carbon dioxide. The mean net carbon uptake for the 12-year period is about 3 tonnes C per hectare, but
with a strong seasonal and interannual variability depending on the weather and water budget. This variability may severely
hamper the accurate quantification of carbon storage by vegetation in our present climates and its projection for future climates. 相似文献
47.
48.
49.
Bert W. Rust Stephen G. Nash Barry J. Geldzahler 《Astrophysics and Space Science》1989,152(1):141-170
Two models for superluminal radio sources predict sharp lower bounds for the apparent velocities of separation. The light echo model predicts a minimum velocityv
min=2c, and the dipole field model predictsv
min=4.446c. Yahil (1979) has suggested that, if either of these models is correct, thenv
min provides a standard velocity which can be used to determine the cosmological parametersH andq
0. This is accomplished by estimating a lower envelope for the proper motion vs redshift relation. Yahil also argued that the procedure could easily be generalized to include a nonzero cosmical constant . We derive the formulas relating the proper motion
to the redshiftz in a Friedmann universe with a nonzero . We show that the determination of a lower envelope for a given sample of measured points
yields an estimate of the angle of inclination
i
for each source in the sample. We formulate the estimation of the lower envelope as a constrained maximum likelihood problem with the constraints specified by the expected value of the largest order statistic for the estimated
i
. We solve this problem numerically using an off-the-shelf nonlinearly constrained nonlinear optimization program from the NAg library. Assuming =0, we apply the estimation procedure to a sample of 27 sources with measured values
, using both the light echo and the dipole field models. The fits giveH=103 km s–1 Mpc–1 for the light echo model andH=46 km s–1 Mpc–1 for the dipole field model. In both cases the fits giveq
0=0.4, but the uncertainty in this result is too large to rule out the possibility thatq
0>0.5. When is allowed to be a free parameter, we obtainH=105 km s–1 Mpc–1 for the light echo model andH=47 km s–1 Mpc–1 for the dipole field model. In both cases the fits giveq
0=–1 and /H
0
2
=6.7, but no significance can be attached to these results because of the paucity of measured data at hight redshifts. For all of the fits, we compute the corresponding estimates of the
i
and compare the cumulative distribution of these values with that expected from a sample of randomly oriented sources. In all cases we find a large excess of sources at low-inclination angles (high apparent velocities). The expected selection effect would produce such an excess, but the excess is large enough to suggest a strong contamination of the sample by relativistic beam sources which would only be seen at low inclination angles.Applied Research Corporation 相似文献
50.
Melanie Beck Jürgen Köster Bert Engelen Jan M. Holstein Antje Gittel Martin Könneke Thomas Riedel Kai Wirtz Heribert Cypionka Jürgen Rullkötter Hans-Jürgen Brumsack 《Ocean Dynamics》2009,59(2):371-383
Microbial activity in permeable tidal flat margin sediments is enhanced by two main processes. First, organic matter is supplied
by rapid sedimentation at prograding tidal flat margins. Second, surface and deep pore water advection lead to a replenishment
of the dissolved organic matter and sulfate pools. Increasing microbial activity towards the low water line is reflected in
sulfate and methane profiles as well as in total cell numbers, sulfate reduction rates, and remineralization products. The
impact of high sedimentation rates on pore water biogeochemistry is confirmed by inverse modeling reproducing the depth profiles
obtained by measurements. In central parts of the tidal flats, low sedimentation rates and pore water flow velocities limit
microbial activity despite the high availability of electron acceptors for microbial respiration such as sulfate. Therefore,
tidal flat margins with high microbial activity are of special importance for budgeting biogeochemical cycling in tidal flat
areas. 相似文献