Catena, ISSN 0341-8162, 04/2019, Volume 175, pp. 77 - 92
The local occurrence of red subsoils on the Late Pleistocene sandy deposits of the Northern European lowlands invites investigation into the formation and...
Soil genesis | Rubification | Soil geography | Catena | Iron oxides | FTIR | LATERAL PODZOLIZATION | FT-IR | WATER RESOURCES | SOIL SCIENCE | FERRIHYDRITE | GEOSCIENCES, MULTIDISCIPLINARY | MAGHEMITE | HEMATITE | GOETHITE | BOG-IRON ORE | OXIDES | IN-SITU | MINERALOGY | Hematite | Soils | Iron compounds | Analysis
Soil genesis | Rubification | Soil geography | Catena | Iron oxides | FTIR | LATERAL PODZOLIZATION | FT-IR | WATER RESOURCES | SOIL SCIENCE | FERRIHYDRITE | GEOSCIENCES, MULTIDISCIPLINARY | MAGHEMITE | HEMATITE | GOETHITE | BOG-IRON ORE | OXIDES | IN-SITU | MINERALOGY | Hematite | Soils | Iron compounds | Analysis
Journal Article
Proceedings of the National Academy of Sciences of the United States of America, ISSN 0027-8424, 11/2008, Volume 105, Issue 46, pp. 17842 - 17847
Soil bacteria regulate wetland biogeochemical processes, yet little is known about controls over their distribution and abundance. Bacteria in North Carolina...
Agricultural soils | Wetland soils | Soil composition | Soil nutrients | Acid soils | Soil bacteria | Land use | Coastal plain soils | Wetlands | Forest soils | Phylogenetic analysis | Soil pH | 16S rDNA | Restoration | BIODIVERSITY | FLORIDA-EVERGLADES | SEDIMENTS | MULTIDISCIPLINARY SCIENCES | MICROBIAL COMMUNITY | RIBOSOMAL-RNA | SPHAGNUM PEAT BOG | phylogenetic analysis | land use | BIOGEOCHEMISTRY | soil pH | DIVERSITY | ECOSYSTEM | restoration | North Carolina | Soil Microbiology | Humans | Molecular Sequence Data | Phylogeny | Bacteria - genetics | Bacteria - classification | RNA, Ribosomal, 16S - genetics | Soil | Fresh Water | Principal Component Analysis | Hydrogen-Ion Concentration | Biogeochemistry | United States | Spatial behavior in animals | Soil acidity | Influence | Research | Soil microbiology | Biological diversity | Biological Sciences
Agricultural soils | Wetland soils | Soil composition | Soil nutrients | Acid soils | Soil bacteria | Land use | Coastal plain soils | Wetlands | Forest soils | Phylogenetic analysis | Soil pH | 16S rDNA | Restoration | BIODIVERSITY | FLORIDA-EVERGLADES | SEDIMENTS | MULTIDISCIPLINARY SCIENCES | MICROBIAL COMMUNITY | RIBOSOMAL-RNA | SPHAGNUM PEAT BOG | phylogenetic analysis | land use | BIOGEOCHEMISTRY | soil pH | DIVERSITY | ECOSYSTEM | restoration | North Carolina | Soil Microbiology | Humans | Molecular Sequence Data | Phylogeny | Bacteria - genetics | Bacteria - classification | RNA, Ribosomal, 16S - genetics | Soil | Fresh Water | Principal Component Analysis | Hydrogen-Ion Concentration | Biogeochemistry | United States | Spatial behavior in animals | Soil acidity | Influence | Research | Soil microbiology | Biological diversity | Biological Sciences
Journal Article
Ecological Monographs, ISSN 0012-9615, 05/2015, Volume 85, Issue 2, pp. 133 - 155
Elemental stoichiometry constitutes an inherent link between biogeochemistry and the structure and processes within food webs, and thus is at the core of...
homeostasis | nutrient recycling | phosphorus deficiency | carbon use efficiency | soil enzymes | litter decomposition | nitrogen turnover | soil microbiology | growth rate hypothesis | substrate age hypothesis | REVIEWS | Stoichiometry | Soil microorganisms | Plant nutrition | Ecosystems | Microbial ecology | Soil nutrients | Plants | Plant litter | Soil ecology | Forest soils | Carbon use efficiency | Soil enzymes | Growth rate hypothesis | Nitrogen turnover | Phosphorus deficiency | Homeostasis | Litter decomposition | Substrate age hypothesis | Nutrient recycling | Soil microbiology | FINE-ROOT PRODUCTION | N-P STOICHIOMETRY | FOLIAR NUTRIENT RESORPTION | SUB-ARCTIC BOG | TERRESTRIAL ECOSYSTEMS | NITROGEN USE EFFICIENCY | CARBON-USE EFFICIENCY | PHOSPHORUS RESORPTION | NEOTROPICAL RAIN-FOREST | ECOLOGY | LEAF-LITTER DECOMPOSITION | Environmental aspects | Nitrogen
homeostasis | nutrient recycling | phosphorus deficiency | carbon use efficiency | soil enzymes | litter decomposition | nitrogen turnover | soil microbiology | growth rate hypothesis | substrate age hypothesis | REVIEWS | Stoichiometry | Soil microorganisms | Plant nutrition | Ecosystems | Microbial ecology | Soil nutrients | Plants | Plant litter | Soil ecology | Forest soils | Carbon use efficiency | Soil enzymes | Growth rate hypothesis | Nitrogen turnover | Phosphorus deficiency | Homeostasis | Litter decomposition | Substrate age hypothesis | Nutrient recycling | Soil microbiology | FINE-ROOT PRODUCTION | N-P STOICHIOMETRY | FOLIAR NUTRIENT RESORPTION | SUB-ARCTIC BOG | TERRESTRIAL ECOSYSTEMS | NITROGEN USE EFFICIENCY | CARBON-USE EFFICIENCY | PHOSPHORUS RESORPTION | NEOTROPICAL RAIN-FOREST | ECOLOGY | LEAF-LITTER DECOMPOSITION | Environmental aspects | Nitrogen
Journal Article
Environmental Science & Technology, ISSN 0013-936X, 02/2018, Volume 52, Issue 4, pp. 1919 - 1928
The application of mineral phosphate (P) fertilizers leads to an unintended Cd input into agricultural systems, which might affect soil fertility and quality...
ENVIRONMENTAL SCIENCES | TRACE-ELEMENTS | FRACTIONATION | PEAT BOG | ENGINEERING, ENVIRONMENTAL | HEAVY-METALS | LEAD ISOTOPES | ATMOSPHERIC DEPOSITION | SOUTHERN NORWAY | LAKE-SEDIMENTS | CADMIUM FLUXES
ENVIRONMENTAL SCIENCES | TRACE-ELEMENTS | FRACTIONATION | PEAT BOG | ENGINEERING, ENVIRONMENTAL | HEAVY-METALS | LEAD ISOTOPES | ATMOSPHERIC DEPOSITION | SOUTHERN NORWAY | LAKE-SEDIMENTS | CADMIUM FLUXES
Journal Article
Plant and Soil, ISSN 0032-079X, 7/2015, Volume 392, Issue 1/2, pp. 345 - 356
Aims To compare growth variability of Scots pine (Pinus sylvestris L.) on different soil types, and to assess the potential of peat-soil pines for...
Life Sciences | Hydrology | Climate change | Regional climate | Meteorological data | Plant Physiology | Ecology | Plant Sciences | Dendrochronology | Soil Science & Conservation | SWEDEN | AGRONOMY | PEATLANDS | PLANT SCIENCES | SOIL SCIENCE | C-14 | FLUCTUATIONS | DYNAMICS | SITES | SCOTS PINE | MOUNTAINS | RADIAL GROWTH | RAISED BOG | Physiological aspects | Scots pine | Research | Analysis | Soil microbiology | Trees | Plant growth | Meteorology | Geography | Humanities and Social Sciences | Biodiversity and Ecology | Environmental Sciences | Climate Research | Miljövetenskap | Naturvetenskap | Klimatforskning | Natural Sciences | Geovetenskap och miljövetenskap | Earth and Related Environmental Sciences
Life Sciences | Hydrology | Climate change | Regional climate | Meteorological data | Plant Physiology | Ecology | Plant Sciences | Dendrochronology | Soil Science & Conservation | SWEDEN | AGRONOMY | PEATLANDS | PLANT SCIENCES | SOIL SCIENCE | C-14 | FLUCTUATIONS | DYNAMICS | SITES | SCOTS PINE | MOUNTAINS | RADIAL GROWTH | RAISED BOG | Physiological aspects | Scots pine | Research | Analysis | Soil microbiology | Trees | Plant growth | Meteorology | Geography | Humanities and Social Sciences | Biodiversity and Ecology | Environmental Sciences | Climate Research | Miljövetenskap | Naturvetenskap | Klimatforskning | Natural Sciences | Geovetenskap och miljövetenskap | Earth and Related Environmental Sciences
Journal Article
Ecosystems, ISSN 1432-9840, 1/2014, Volume 17, Issue 1, pp. 112 - 126
Knowledge on soil microbial respiration (SMR) rates and thus soil-related CO₂ losses from Arctic soils is vital because of the crucial importance of this...
Tundras | Peat soils | Soil quality | Permafrost | Mineral soils | Tundra soils | Soil respiration | Peat | Organic soils | Forest soils | trenching | CO 2 | bioavailability of soil carbon | Zoology | microbial respiration | upland soils | isotope partitioning | soil respiration | Ecology | Life Sciences | Nature Conservation | Geoecology/Natural Processes | peat soils | subarctic tundra | Plant Sciences | Environmental Management | ECOSYSTEM RESPIRATION | PERMAFROST THAW | TURNOVER | EMISSIONS | CO2 | OLD CARBON | COMPONENTS | TUNDRA ECOSYSTEMS | CO2 EXCHANGE | ORGANIC-CARBON | ECOLOGY | VEGETATION | Soils | Carbon content | Nuclear radiation | Ecosystems | Analysis | Soil microbiology | Peat-bogs | Atmospheric carbon dioxide | Studies | Carbon cycle | Grasslands | Soil microorganisms | Soil mechanics
Tundras | Peat soils | Soil quality | Permafrost | Mineral soils | Tundra soils | Soil respiration | Peat | Organic soils | Forest soils | trenching | CO 2 | bioavailability of soil carbon | Zoology | microbial respiration | upland soils | isotope partitioning | soil respiration | Ecology | Life Sciences | Nature Conservation | Geoecology/Natural Processes | peat soils | subarctic tundra | Plant Sciences | Environmental Management | ECOSYSTEM RESPIRATION | PERMAFROST THAW | TURNOVER | EMISSIONS | CO2 | OLD CARBON | COMPONENTS | TUNDRA ECOSYSTEMS | CO2 EXCHANGE | ORGANIC-CARBON | ECOLOGY | VEGETATION | Soils | Carbon content | Nuclear radiation | Ecosystems | Analysis | Soil microbiology | Peat-bogs | Atmospheric carbon dioxide | Studies | Carbon cycle | Grasslands | Soil microorganisms | Soil mechanics
Journal Article
Journal of Plant Nutrition and Soil Science, ISSN 1436-8730, 06/2006, Volume 169, Issue 3, pp. 310 - 329
Silicon (Si) is the second‐most abundant element in the earth's crust. In the pedosphere, however, huge spans of Si contents occur mainly caused by Si...
phytoliths | silicon | biogenic Si | Si fluxes / biogeosystems | pedogenesis | Pedogenesis | Phytoliths | Silicon | Si fluxes | Biogeosystems | Biogenic Si | GEOCHEMICAL MASS-BALANCE | AGRONOMY | NEW-ZEALAND | peclogenesis | PEAT BOG | LATERAL PODZOLIZATION | ORGANIC-MATTER | QUATERNARY MARINE TERRACES | PLANT SCIENCES | SOIL SCIENCE | CHEMICAL-WEATHERING RATES | biogeosystems | PROTO-IMOGOLITE ALLOPHANE | BIOGENIC OPAL | TEMPERATE FOREST
phytoliths | silicon | biogenic Si | Si fluxes / biogeosystems | pedogenesis | Pedogenesis | Phytoliths | Silicon | Si fluxes | Biogeosystems | Biogenic Si | GEOCHEMICAL MASS-BALANCE | AGRONOMY | NEW-ZEALAND | peclogenesis | PEAT BOG | LATERAL PODZOLIZATION | ORGANIC-MATTER | QUATERNARY MARINE TERRACES | PLANT SCIENCES | SOIL SCIENCE | CHEMICAL-WEATHERING RATES | biogeosystems | PROTO-IMOGOLITE ALLOPHANE | BIOGENIC OPAL | TEMPERATE FOREST
Journal Article
Soil Biology and Biochemistry, ISSN 0038-0717, 03/2018, Volume 118, Issue C, pp. 156 - 160
Although it is generally assumed that CH production in peatlands is dominated by the acetoclastic and hydrogenotrophic methanogenic pathways, we found evidence...
Methane | Methylotrophic | Bog | Isotopes | Methanogenesis | Wetlands | PATHWAYS | BACTERIA | SEDIMENTS | ZOIGE WETLAND | HYDROGEN | SOIL SCIENCE | METABOLISM | COMMUNITY | SULFATE | METHANE PRODUCTION | ACETATE | Agriculture
Methane | Methylotrophic | Bog | Isotopes | Methanogenesis | Wetlands | PATHWAYS | BACTERIA | SEDIMENTS | ZOIGE WETLAND | HYDROGEN | SOIL SCIENCE | METABOLISM | COMMUNITY | SULFATE | METHANE PRODUCTION | ACETATE | Agriculture
Journal Article
Ecosystems, ISSN 1432-9840, 3/2012, Volume 15, Issue 2, pp. 213 - 229
Recent warming at high-latitudes has accelerated permafrost thaw in northern peatlands, and thaw can have profound effects on local hydrology and ecosystem...
Bog soils | Sedimentary soils | Bogs | Peat soils | Peatlands | Soil water | Soil organic matter | Permafrost | Peat | Forest soils | thermokarst | Zoology | soil carbon | boreal | Ecology | Life Sciences | Nature Conservation | Geoecology/Natural Processes | permafrost | peatlands | Alaska | Plant Sciences | Environmental Management | climate change | BOREAL PEATLANDS | WESTERN CANADA | CLIMATE-CHANGE | DISCONTINUOUS PERMAFROST | INTERIOR ALASKA | FIRE | DEGRADATION | ECOLOGY | ACCUMULATION | ECOSYSTEMS | CYCLE | Soils | Hydrology | Carbon content | Global temperature changes | Arctic research | Ecosystems | Analysis | Climatic changes | Universities and colleges | Peat-bogs | Wetlands | Climate change | Carbon | Mosses
Bog soils | Sedimentary soils | Bogs | Peat soils | Peatlands | Soil water | Soil organic matter | Permafrost | Peat | Forest soils | thermokarst | Zoology | soil carbon | boreal | Ecology | Life Sciences | Nature Conservation | Geoecology/Natural Processes | permafrost | peatlands | Alaska | Plant Sciences | Environmental Management | climate change | BOREAL PEATLANDS | WESTERN CANADA | CLIMATE-CHANGE | DISCONTINUOUS PERMAFROST | INTERIOR ALASKA | FIRE | DEGRADATION | ECOLOGY | ACCUMULATION | ECOSYSTEMS | CYCLE | Soils | Hydrology | Carbon content | Global temperature changes | Arctic research | Ecosystems | Analysis | Climatic changes | Universities and colleges | Peat-bogs | Wetlands | Climate change | Carbon | Mosses
Journal Article