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Titlebook: Ecosystem Organization of a Complex Landscape; Long-Term Research i Otto Fr?nzle,Ludger Kappen,Klaus Dierssen Book 2008 Springer-Verlag Ber

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樓主: 弄混
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發(fā)表于 2025-3-23 10:17:04 | 只看該作者
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發(fā)表于 2025-3-23 15:19:52 | 只看該作者
Momentum and Contrarian Strategyractions between these sub-systems, has substantiated the conception that a thorough knowledge of the ecosystem and its unifying position between ecology and environmental science is essential for a coherent understanding of environmental issues and large-scale problems in the biosphere. Recent deve
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發(fā)表于 2025-3-23 22:53:01 | 只看該作者
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發(fā)表于 2025-3-24 03:53:14 | 只看該作者
Maria Grazia Starita,Irma Malafrontehis energy is converted into heat and dissipated by long-wave radiation and convection or is used for the evapotranspiration of water. Only a small fraction of global radiation is used in the process of photosynthesis and changed into chemical energy stored in carbohydrates. Carbon assimilation init
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發(fā)表于 2025-3-24 07:50:41 | 只看該作者
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發(fā)表于 2025-3-24 12:00:05 | 只看該作者
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發(fā)表于 2025-3-24 18:12:25 | 只看該作者
Capital Structure in the Modern World, the irregular habitat pattern may be inducive to higher biodiversity, on the other isolation of habitats may result in a decrease in species numbers, if extinction is not compensated by immigration. In fractal landscape models, the number of species coexisting in microsites increased up to the fra
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發(fā)表于 2025-3-24 21:17:36 | 只看該作者
https://doi.org/10.1007/978-1-349-15773-0e components can be complex and counter-intuitive; for example, groundwater flow can bypass riparian zones, as the following Chapters will show. Therefore, quantitative landscape- scale evaluations of element fluxes are difficult. They require models capable of depicting internal and input/output el
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發(fā)表于 2025-3-24 23:56:21 | 只看該作者
Conclusion: A High-Water Mark?,th respect to the physics of such flow processes, two theoretical approaches are distinguished in general. Using Euler’s concept, the multidimensional partial flow transport equations are solved simultaneously for all points in space at a given time. Lagrange’s approach describes mainly the temporal
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