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SJOERD BOHNCKE LEX WIJMSTRA JAN VAN DER WOUDE HENNY SOHL 《Boreas: An International Journal of Quaternary Research》1988,17(3):385-402
Pollen analyses of three Late Weichselian Late-Glacial lake sediment successions provided a basis for the construction of pollen assemblage zones for The Netherlands. Special attention is paid to the behaviours of Populus in the Alleröd boreal forest. Some aspects of the autecology of Juniperus and Hippohaë and the dynamics of birch and pine forests are discussed in the light of the observed succession. The Late-Glacial vegetational succession in The Netherlands is compared with data published for neighbouring NW European countries. It is concluded that differences in precipitation (snow cover) along a west-east transect to a great extent determined the inferred differences in vegetational development. 相似文献
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Information on the rates, characteristics, and drivers of land‐use change are vital for addressing the impacts and feedbacks of change on environmental processes. The U.S. Geological Survey's Land Cover Trends project is conducting a consistent, national analysis of the rates, causes, and consequences of land‐use change. In this article we assess change in the Atlantic Coastal Pine Barrens ecoregion from 1973 to 2000. Urban lands expanded by more than 900 square kilometers during the study period. Land‐use change in the ecoregion followed the tenets of “Forest Transition Theory” (ftt ) prior to the study period, but forest lands experienced consistent declines from 1973 to 2000. Increasing government regulation during the study period, consistent with concept of the “Quiet Revolution” (qr ), mitigated forest loss during the latter half of the study period. Generalized theories, including ftt and the qr , are valuable, but local and regional determinants of comparative land rents ultimately drive land‐use change at this scale. 相似文献
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Abstract— We present a numerical simulation technique for the retrieval of the electric properties relative permittivity and conductivity of planetary, asteroid, and cometary regolith. Our simulation techniques aim at accompanying hardware development and conducting virtual experiments, e.g., to assess the response of arbitrary heterogeneous conductivity and permittivity distributions or to scrutinize possibilities for spatial reconstruction methods using inverse schemes. In a first step, we have developed a finite element simulation code on the basis of unstructured, adaptive triangular grids for arbitrary two‐dimensional axisymmetric distributions of conductivity and permittivity. The code is able to take into account the spatial geometry of the probe and allows for possible inductive effects. In previous studies, the non‐inductive approach has been used to convert potential and phase data into apparent material properties. By our simulations, we have shown that this approach is valid for the frequency range from 102 Hz to 107 Hz and electric conductivities of 10?8 S/m that are typical for the near‐surface region of asteroids and comets composed of chondritic materials and/or frozen volatiles such as H2O and CO2 ice. We prove the accuracy of our code to be better than 10%, using mixed types of boundary conditions and present a simulated vertical log through a horizontally stratified subsurface layer as a representative example of a heterogeneous distribution of the electrical properties. Resolution studies for the given electrode separation reveal that the material parameters of layers having thicknesses of less than about half the electrode spread are not reconstructible if only apparent quantities are considered. Therefore, spatial distributions of the complex sensitivity are presented having in mind a future data inversion concept that will permit the multi‐dimensional reconstruction of material parameters in heterogeneous environments. 相似文献
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