Soil structure determines a large part of the spatial heterogeneity in water storage and fluxes from the plot to the hillslope scale. In recent decades important progress in hydrological research has been achieved by including soil structure in hydrological models. One of the main problems herein remains the difficulty of measuring soil structure and quantifying its influence on hydrological processes. As soil structure is very often of biogenic origin (macropores), the main objective of this project is to use the influence of bioactivity and resulting soil structures to describe and support modelling of hydrological processes at different scales. Therefore, local scale bioactivity will be linked to local infiltration patterns under varying catchment conditions. At hillslope scale, the spatial distribution of bioactivity patterns will be linked to connectivity of subsurface structures to explain subsurface stormflow generation. Then we will apply species distribution modelling of key organisms in order to extrapolate the gained knowledge to the catchment scale. As on one hand, bioactivity influences the hydrological processes, but on the other hand the species distribution also depends on soil moisture contents, including the feedbacks between bioactivity and soil hydrology is pivotal for getting reliable predictions of catchment scale hydrological behavior under land use change and climate change.
The project is part of the COST action FP0603 Forest models for research and decision support in sustainable forest management (http://www.cost.esf.org/index.php?id=143&action number=FP0603) which aims at extending the scope of forest models from growth only to population dynamics and ecophysiology. Rationale: For sustainable forest management over large areas and for simulating different forest functions especially under changing conditions, different aspects of the system forest' must be modelled jointly: ecophysiological/biogeochemical processes, population dynamics, spatial interactions, and horizontal/vertical species stand structure. We develop a forest model with a stand-size grain suitable to be applied on large areas for assessment of, e.g., climate change or management effects on forest functions. This is achieved by merging and if necessary up- and down-scaling model functions of ecophysiological and population dynamical processes contained in existing models (single tree physiology, local scale ecophysiological, empirical forest growth, spatio-temporal forest landscape, and dynamic global vegetation models). Drought is predicted to occur more frequently with climate change, thus the main focus is on drought and the mechanisms how it affects the trees. Research questions: What are the mechanisms by which drought affects trees? Which is the best (sufficiently accurate and efficient) way to model and simulate these mechanisms? How can population dynamics and ecophysiology be combined in a landscape scale model concerning - allocation of water and carbohydrates to trees and organs? - spatial heterogeneity of soil water and trees? Methods: The project builds on the climate-driven forest landscape model TreeMig (Lischke et al., 2006). Process descriptions from various existing models are compiled, evaluated and included into TreeMig. This involves a thorough scaling of process formulations. Drought effects, involving soil water balance, stomata regulation, photosynthesis, CO2 fertilization effects, allocation of carbohydrates, dynamics of reserve pools and the relationship between these and regeneration, growth and mortality are studied in literature and other models and included into MEPHYSTO.
Beim Regionalen Raumordnungsprogramm (RROP) handelt es sich um ein strategisches Instrument zur räumlichen Steuerung, Ordnung der unterschiedlichen Nutzungsansprüche. Dabei sollen die miteinander konkurrierenden raumbezogenen Planungen, wie beispielsweise Land- und Forstwirtschaft, gewerbliche Wirtschaft, Verkehr, Naturschutz, Wohnraumbedarf u.v.m aufeinander abgestimmt werden. Das RROP ist somit auf der Ebene des Landkreises ein übergeordnetes und zusammenfassendes Planwerk. Basis für die Vielfalt an Themen bildet das Raumordnungsprogramm 2003 mit der 1. Änderung 2010.
Der interoperable INSPIRE-Datensatz beinhaltet Daten vom LBGR über die Hydrogeologische Raumgliederung Brandenburg, transformiert in das INSPIRE-Zielschema Geologie. Der Datensatz wird über je einen interoperablen Darstellungs- und Downloaddienst bereitgestellt. --- The compliant INSPIRE data set contains data about the hydrogeological spatial classification in the State of Brandenburg from the LBGR, transformed into the INSPIRE target schema Geology. The data set is provided via compliant view and download services.
Kartenverzeichnis des rechtskräftigen Regionalplanes in der Fassung der Bekanntmachung vom 16.08.2007: Karte 1 Raumstruktur (1:280 000) Karte 2 Raumnutzung (1:100 000) Karte 3 Siedlungswesen (1:280 000) Karte 4 Zentrale Orte - Lage im Raum (1:280 000) Karte 5 Zentrale Orte - administrative Gliederung (1:280 000) Karte 6 Naturräumliche Gliederung (1:280 000) Karte 7 Kulturlandschaftlich bedeutsame Bereiche (1:280 000) Karte 8 Schutzgebiete nach Naturschutzrecht (1:100 000) Karte 9 Natura 2000 (1:280 000) Karte 10 Windenergienutzung (1:280 000) Karte 11 Sanierungsbedürftige Bereiche der Landschaft/Landschaftspflege (1:200 000) Karte 12 Bergbauumgang (1:280 000) Karte 13 Tierhaltungsstandorte (1:280 000) Karte 14 Tourismus und Erholung (1:280 000)
Inhaltsverzeichnis des Kartenteils der ersten Gesamtfortschreibung des Regionalpla-nes für die Anhörung entsprechend Sächsisches Landesplanungsgesetz (SächsLPlG): Karte 1 Raumnutzung (1:100 000) Karte 2 Siedlungswesen (1:280 000) Karte 3 Raumstruktur (1:280 000) Karte 4 Tourismus (1:280 000) Karte 5 Landschaftsbereiche mit besonderen Nutzungsanforderungen (1:200 000) Karte 6 Sanierungsbedürftige Bereiche der Landschaft (1:200 000) Karte 7 Tierhaltungsstandorte (1:280 000) Karte 8 Bergbauumgang (1:280 000)
Inhaltsverzeichnis des Kartenteils der ersten Gesamtfortschreibung des Regionalplanes für die Anhörung entsprechend Sächsisches Landesplanungsgesetz (SächsLPlG): Karte 1 Karte "Zentrale Orte und Nahbereiche" (Erläuterungskarte) (1:400 000) Karte 2 Karte "Raumstruktur" (Festlegungskarte) (1:400 000) Karte 3 Karte "Freizeit, Erholung, Tourismus" (Erläuterungskarte) (1:200 000) Karte 4 Karte "Straßennetzausbau" (Erläuterungskarte) (1:400 000) Karte 5 Karte "Sorbisches Siedlungsgebiet" (Erläuterungskarte) (1:400 000) Karte 6 Karte "Ökologisches Verbundsystem und regionale Grünzüge" (Festlegungskarte) (1:100 000) Karte 7 Karte "Landschaftspflege, -sanierung und -entwicklung" (Festlegungskarte) (1:100 000) Karte 8 Karte "Raumnutzung" (Festlegungskarte) Kartenteil zu Anhang 4 (Fachplanerische Inhalte des Landschaftsrahmenplans) Karte "Naturräumliche Gliederung der Region" (1:400 000) Karte "Integriertes Entwicklungskonzept" (1:100 000)
Seagrass meadows provide valuable socio-ecological ecosystem services, including a key role in climate change mitigation and adaption. Understanding the natural history of seagrass meadows across environmental gradients is crucial to decipher the role of seagrasses worldwide. This database comprises of data compiled from peer-previewed publications (1975-2020; based on a Web of Science search) containing 11 individual measures of seagrass meadow structure (e.g. percent cover), biomass (e.g. above-ground biomass) and productivity (e.g. shoot production). Each row of data also includes biological, spatial and temporally relevant information such as bioregion, latitude, longitude, sampling year and genera. This compiled database will facilitate a deeper understanding of spatial and temporal patterns in seagrass meadow structure, biomass and production characteristics globally.
The pattern of plant nutrient uptake in a soil profile is the result of complex processes occurring at the cellular or sub-cellular levels but affecting the whole-plant behaviour in function of the plant environment that varies strongly in time and space. The plant nutrient acquisition depends on root architecture and growth, on soil properties and heterogeneity, and on the 3-D distribution of nutrients and water. Equally important is how these parameters interact, as for instance how the nutrient distribution and soil properties and heterogeneity impact root growth or how nutrient and water limitation affect assimilate allocation. Mathematical modelling using a spatial resolution that resolves the spatial structure of the root structure and the nutrient and water distribution is therefore needed to quantitatively account for these complex and interacting processes and to predict plant nutrient uptake behaviour under environmental constraints. The main goal of the project is to build a modelling platform able to describe 3-D flow and transport processes in the soil to individual roots of an entire root system (WP1). Model parameters will be derived from specific experiments performed at the plant scale in the research group (WP3) and stored in a specific data warehouse (WP2). The impact of different parameters, which describe root growth and nutrient uptake at the single root scale, on nutrient uptake at the soil profile scale, will be investigated based on scenario analyses (WP4). Data on water and nutrient uptake and root growth from plant and field scale experiments will be compared with model predictions to validate the model. Simulations with the 3-D root scale model will be used to validate hypotheses and parameterizations of larger scale 1-D models that do not describe processes at the scale of individual roots (WP5 and SP10).
Der Datensatz beinhaltet Daten vom LBGR über die Hydrogeologische Raumgliederung Brandenburgs und wird über je einen Darstellungs- und Downloaddienst bereitgestellt. Die Karte gibt einen Überblick zu den hydrogeologischen Raumgliederungen Brandenburgs. Die Gliederungseinheiten tragen den angewandten Charakter von Nutzungsräumen. Sie werden anhand von Wassereinzugsgebieten und Charakteristiken dazugehöriger Grundwasserdynamik beschrieben. Für das Territorium einer hydrogeologischen Einheit werden vergleichbare Grundwasserverhältnisse vorausgesetzt.
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