feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    UID:
    edoccha_BV047690996
    Format: 1 Online-Ressource (XIII, 414 Seiten) : , Illustrationen.
    ISBN: 978-3-030-83225-4
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83224-7
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83226-1
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83227-8
    Language: English
    URL: Volltext  (URL des Erstveröffentlichers)
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
  • 2
    UID:
    edocfu_BV047690996
    Format: 1 Online-Ressource (XIII, 414 Seiten) : , Illustrationen.
    ISBN: 978-3-030-83225-4
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83224-7
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83226-1
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83227-8
    Language: English
    URL: Volltext  (URL des Erstveröffentlichers)
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
  • 3
    UID:
    gbv_1794571825
    Format: 1 Online-Ressource (120 p.)
    ISBN: 9782889635481
    Content: Soil fauna plays a significant role at all trophic levels of the soil food web and regulates processes that are crucial for soil functioning, such as nutrient cycling, immobilization and/or degradation of toxic compounds, formation of soil structure, greenhouse gas emissions and C turnover. Although soil fauna is not thought to contribute significantly to soil respiration during litter or soil organic matter (SOM) decomposition, the diversity of soil fauna has been found to strongly influence SOM distribution and dynamics. Yet, the functional contribution of soil fauna to many soil processes is not well understood due to methodological limitations and the high complexity of interactions at various spatiotemporal scales. In general, soil fauna has received far less scientific attention than bacteria and fungi (and lately archaea) in soil studies and has been regularly ignored in global biogeochemical models, with maybe exceptions for some earthworms. However, recent studies are raising the awareness of the influence of soil fauna on ecosystems dynamics. For instance, earthworms have been found to be major players in N2O emissions from soils. They exert a strong influence on C stabilization, and they promote the degradation of polycyclic aromatic hydrocarbons (PAHs). Less studied, ants and termites have been found to increase crop productivity in drylands, and different lifeforms of Collembola have been shown to impact microorganisms in various ways over time, thereby potentially affecting C and N cycles within farming systems. The influence of soil fauna indeed manifests over a broad ranges of spatiotemporal scales. For example, some effect such as aggregate formation may cumulate over time and finally contribute to the formation of whole soil profiles, which serve as a framework for other soil processes such as water movement, decomposition, etc. Meanwhile, soil biodiversity is impacted by an increasing human pressure through deforestation, agriculture intensification, habitat fragmentation or climate change (increasing temperatures, extreme weather events), which leads to soil biodiversity loss, in particular of soil fauna, with associated consequences on soil functioning and resilience
    Note: English
    Language: English
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
  • 4
    UID:
    b3kat_BV047690996
    Format: 1 Online-Ressource (XIII, 414 Seiten) , Illustrationen
    ISBN: 9783030832254
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83224-7
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83226-1
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83227-8
    Language: English
    URL: Volltext  (URL des Erstveröffentlichers)
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
  • 5
    UID:
    almafu_BV047690996
    Format: 1 Online-Ressource (XIII, 414 Seiten) : , Illustrationen.
    ISBN: 978-3-030-83225-4
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83224-7
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83226-1
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 978-3-030-83227-8
    Language: English
    URL: Volltext  (URL des Erstveröffentlichers)
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
  • 6
    Online Resource
    Online Resource
    Prague :Karolinum Press,
    UID:
    almafu_9959234596302883
    Format: 1 online resource (94 pages)
    Edition: 1st ed.
    ISBN: 80-246-3822-3
    Note: Obálka -- Obsah -- 1 Úvod -- 2 O poznání a o sdělení -- 3 Odborné publikace -- 3.1 Co je publikace -- 3.2 Druhy odborných publikací -- 3.3 Struktura hlavních typů publikací a jak je číst -- 4 Studium odborné literatury -- 4.1 Proč a jak čteme odborný text -- 4.1.1 Proč a jak čteme odborný text - příklad -- 4.1.2 Odbornou literaturu čteme na základě plánu -- 4.1.3 Odbornou literaturu čteme z nějakého důvodu -- 4.1.4 Odbornou literaturu čteme kreativně -- 4.2 Plánujeme četbu podle našeho cíle -- 4.3 Hledáme zdroje -- 4.4 Jak sehnat práce, které potřebujeme přečíst -- 4.5 Jak číst -- 5 Píšeme odborný text -- 5.1 Píšeme rešerši -- 5.1.1 Příprava textu -- 5.1.2 Psaní -- 5.1.3 Kontrola a opravy textu -- 5.2 Píšeme originální článek z původních dat -- 5.2.1 Posíláme článek a komunikujeme s redakcí recenzovaného časopisu -- 5.3 Další formy vědeckých sdělení -- 6 Slovo závěrem -- 7 Summary -- 8 Literatura -- 9 Rejstřík.
    Additional Edition: ISBN 80-246-3815-0
    Language: Czech
    Keywords: Electronic books.
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
  • 7
    Online Resource
    Online Resource
    Boca Raton :Taylor & Francis,
    UID:
    almahu_9949319963002882
    Format: 1 online resource (315 pages) : , illustrations (some color)
    ISBN: 9781466599338 (e-book)
    Content: "Mining supplies numerous raw minerals that are essential for economic development. In many cases, however, mineral extraction causes severe destruction of the environment. Large areas can be literally erased by excavation and dumping of overburden. In addition, mining and postprocessing of raw materials may accelerate weathering processes and chemically alter the environment through, for example, acidification or pollution by heavy metals. Environmental damage brings the necessity for ecosystem reconstruction in affected areas. Numerous approaches to land reclamation have been developed. Natural processes collectively referred to as ecological succession, however, bring about gradual ecosystem development without the assistance of man. These processes may be relatively slow, particularly in their early stages, but there are many examples of how they have led to the development of functional ecosystems in the long-term, typically after several decades. In this book, we pay attention to the study of these successional processes. Firstly, only comparisons between the results of reclamation technologies and those of natural succession at unreclaimed sites of the same age can provide us with real information about the added value of reclamation. Secondly, a better understanding of natural succession processes may inspire numerous future improvements to restoration technologies. Finally, post-mining sites represent an excellent model for studying succession processes and may substantially improve our knowledge about these ecological phenomena"--Provided by publisher.
    Note: "A CRC title, part of the Taylor & Francis imprint, a member of the Taylor & Francis Group, the academic division of T&F Informa plc." , Geological Substrates and Heaping Process of Coal Mining Operations in the Sokolov Basin, Czech Republic : Implications for Reclamation and Soil Development / Petr Rojík -- Humus Accumulation and Humification during Soil Development in Post-Mining Soil / Evgenij Abakumov and Jan Frouz -- Vegetation Development in Central European Coal Mining Sites / Karel Prach -- Biological Soil Crusts in Post-Mining Areas / Alena Lukešová, Martina Zahradníková and Jan Frouz -- Soil Properties and Development of Humus Forms in Pine and Oak Stands of Reclaimed Post-mining Sites in Lusatia : Influence of Lignite from Overburden Sediments and Dust Immissions / Oliver Bens and Reinhard F. Hüttl -- Plant Production, Carbon Accumulation and Soil Chemistry at Post-Mining Sites / Jan Frouz, Petr Dvoršćík, Olga Vindušková and Emil Cienciala -- Soil Microflora Development in Post-mining Sites / Jan Frouz, Dana Elhottová, Petr Baldrián, Alice Chronáková, Alena Lukešová, Alena Nováková and Václav Krištůfek -- Macrofungi in Post-mining Sites / Lucie Zíbarová and Anna Lepšová -- Interactions of Plants with Arbuscular Mycorrhizal Fungi during Ecosystem Development at Post Mining Sites in the Most Coal Basin (Czech Republic) / Jana Rydlová, David Püschel, Martina Janoušková and Miroslav Vosátka -- Recovery and Colonization at Post-mining Sites by the Soil Microfauna / L. Hánel, M. Devetter and S. Adl -- Soil Macro- and Mesofauna Succession in Post-mining Sites and Other Disturbed Areas / Jan Frouz, Václav Pižl, Karel Tajovský, Josef Starý, Michal Holec and Jan Materna -- The Role of Soil Macrofauna in Soil Formation and Carbon Storage in Post-mining Sites / Jan Frouz -- Soil Fauna Plant Interactions during Succession at Post-mining Sites / A. Roubícková, O. Mudrák and J. Frouz -- Soil Fauna and Soil Physical Properties / Jan Frouz and V. Kuráž -- Mining Land and Similar Habitats : A Barren Land or a New Wilderness in the Cultural Landscape? / Tomás Gremlica -- Soil Biota and Ecosystem Development in Post-Mining Sites : Conclusions and Practical Implications / Jan Frouz.
    Additional Edition: Print version: Soil biota and ecosystem development in post mining sites. Boca Raton : Taylor & Francis, [2014] ISBN 9781466599314
    Language: English
    Keywords: Electronic books. ; Aufsatzsammlung
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
  • 8
    UID:
    almahu_9949281413602882
    Format: 1 electronic resource (120 p.)
    Content: Soil fauna plays a significant role at all trophic levels of the soil food web and regulates processes that are crucial for soil functioning, such as nutrient cycling, immobilization and/or degradation of toxic compounds, formation of soil structure, greenhouse gas emissions and C turnover. Although soil fauna is not thought to contribute significantly to soil respiration during litter or soil organic matter (SOM) decomposition, the diversity of soil fauna has been found to strongly influence SOM distribution and dynamics. Yet, the functional contribution of soil fauna to many soil processes is not well understood due to methodological limitations and the high complexity of interactions at various spatiotemporal scales. In general, soil fauna has received far less scientific attention than bacteria and fungi (and lately archaea) in soil studies and has been regularly ignored in global biogeochemical models, with maybe exceptions for some earthworms. However, recent studies are raising the awareness of the influence of soil fauna on ecosystems dynamics. For instance, earthworms have been found to be major players in N2O emissions from soils. They exert a strong influence on C stabilization, and they promote the degradation of polycyclic aromatic hydrocarbons (PAHs). Less studied, ants and termites have been found to increase crop productivity in drylands, and different lifeforms of Collembola have been shown to impact microorganisms in various ways over time, thereby potentially affecting C and N cycles within farming systems. The influence of soil fauna indeed manifests over a broad ranges of spatiotemporal scales. For example, some effect such as aggregate formation may cumulate over time and finally contribute to the formation of whole soil profiles, which serve as a framework for other soil processes such as water movement, decomposition, etc. Meanwhile, soil biodiversity is impacted by an increasing human pressure through deforestation, agriculture intensification, habitat fragmentation or climate change (increasing temperatures, extreme weather events), which leads to soil biodiversity loss, in particular of soil fauna, with associated consequences on soil functioning and resilience.
    Note: English
    Additional Edition: ISBN 2-88963-548-1
    Language: English
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
  • 9
    UID:
    edocfu_9960408199302883
    Format: 1 electronic resource (120 p.)
    Content: Soil fauna plays a significant role at all trophic levels of the soil food web and regulates processes that are crucial for soil functioning, such as nutrient cycling, immobilization and/or degradation of toxic compounds, formation of soil structure, greenhouse gas emissions and C turnover. Although soil fauna is not thought to contribute significantly to soil respiration during litter or soil organic matter (SOM) decomposition, the diversity of soil fauna has been found to strongly influence SOM distribution and dynamics. Yet, the functional contribution of soil fauna to many soil processes is not well understood due to methodological limitations and the high complexity of interactions at various spatiotemporal scales. In general, soil fauna has received far less scientific attention than bacteria and fungi (and lately archaea) in soil studies and has been regularly ignored in global biogeochemical models, with maybe exceptions for some earthworms. However, recent studies are raising the awareness of the influence of soil fauna on ecosystems dynamics. For instance, earthworms have been found to be major players in N2O emissions from soils. They exert a strong influence on C stabilization, and they promote the degradation of polycyclic aromatic hydrocarbons (PAHs). Less studied, ants and termites have been found to increase crop productivity in drylands, and different lifeforms of Collembola have been shown to impact microorganisms in various ways over time, thereby potentially affecting C and N cycles within farming systems. The influence of soil fauna indeed manifests over a broad ranges of spatiotemporal scales. For example, some effect such as aggregate formation may cumulate over time and finally contribute to the formation of whole soil profiles, which serve as a framework for other soil processes such as water movement, decomposition, etc. Meanwhile, soil biodiversity is impacted by an increasing human pressure through deforestation, agriculture intensification, habitat fragmentation or climate change (increasing temperatures, extreme weather events), which leads to soil biodiversity loss, in particular of soil fauna, with associated consequences on soil functioning and resilience.
    Note: English
    Additional Edition: ISBN 2-88963-548-1
    Language: English
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
  • 10
    UID:
    edoccha_9960408199302883
    Format: 1 electronic resource (120 p.)
    Content: Soil fauna plays a significant role at all trophic levels of the soil food web and regulates processes that are crucial for soil functioning, such as nutrient cycling, immobilization and/or degradation of toxic compounds, formation of soil structure, greenhouse gas emissions and C turnover. Although soil fauna is not thought to contribute significantly to soil respiration during litter or soil organic matter (SOM) decomposition, the diversity of soil fauna has been found to strongly influence SOM distribution and dynamics. Yet, the functional contribution of soil fauna to many soil processes is not well understood due to methodological limitations and the high complexity of interactions at various spatiotemporal scales. In general, soil fauna has received far less scientific attention than bacteria and fungi (and lately archaea) in soil studies and has been regularly ignored in global biogeochemical models, with maybe exceptions for some earthworms. However, recent studies are raising the awareness of the influence of soil fauna on ecosystems dynamics. For instance, earthworms have been found to be major players in N2O emissions from soils. They exert a strong influence on C stabilization, and they promote the degradation of polycyclic aromatic hydrocarbons (PAHs). Less studied, ants and termites have been found to increase crop productivity in drylands, and different lifeforms of Collembola have been shown to impact microorganisms in various ways over time, thereby potentially affecting C and N cycles within farming systems. The influence of soil fauna indeed manifests over a broad ranges of spatiotemporal scales. For example, some effect such as aggregate formation may cumulate over time and finally contribute to the formation of whole soil profiles, which serve as a framework for other soil processes such as water movement, decomposition, etc. Meanwhile, soil biodiversity is impacted by an increasing human pressure through deforestation, agriculture intensification, habitat fragmentation or climate change (increasing temperatures, extreme weather events), which leads to soil biodiversity loss, in particular of soil fauna, with associated consequences on soil functioning and resilience.
    Note: English
    Additional Edition: ISBN 2-88963-548-1
    Language: English
    Library Location Call Number Volume/Issue/Year Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. Further information can be found on the KOBV privacy pages