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  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Stream ecology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (447 pages)
    Edition: 1st ed.
    ISBN: 9780080517995
    Series Statement: Aquatic Ecology Series
    Language: English
    Note: Front Cover -- Streams and Ground Waters -- Copyright Page -- Contents -- Contributors -- Preface -- SECTION ONE: THE PHYSICAL TEMPLATE: HYDROLOGY, HYDRAULICS, AND PHYSICAL STRUCTURE -- Chapter 1. Quantifying Hydrologic Interactions between Streams and Their Subsurface Hyporheic Zones -- I. Introduction -- II. Challenge of Investigating Small-Scale Subsurface Processes That May Have Basin-Scale Consequences -- III. Empirical Approaches to Quantifying Hydrologic Exchange between Streams and Shallow Ground Water -- IV. Using the Stream-Tracer Approach to Characterize the Hyporheic Zone -- V. Paradigm Lost? Limitations of the Stream-Tracer Approach as a Means to Quantify Hyporheic Processes -- VI. Charting New Directions in Hyporheic-Zone Research -- VII. Conclusion -- References -- Chapter 2. Modeling Surface-Subsurface Hydrologic Interactions -- I. Introduction -- II. Viewing the Interaction from the Stream -- III. Viewing the Interaction from the Stream-Bed Interface -- IV. Viewing the Interaction from the Subsurface -- V. Challenges -- References -- SECTION TWO: BIOGEOCHEMISTRY SUBSYSTEM INTERACTIONS WITH STREAM SURFACE WATER -- Chapter 3. Stream Chemistry and Riparian Zones -- I. Introduction -- II. Riparian Zone Hydrological-Chemical Interactions: An Overview -- III. Riparian Influences on Stream Chemistry -- IV. Riparian Zone Influences on Stream Chemistry in Relation to Watershed Hydrogeology: A Conceptual Framework -- V. Future Research Directions -- References -- Chapter 4. Flood Frequency and Stream-Riparian Linkages in Arid Lands -- I. Introduction -- II. Riparian Zones in Arid Catchments -- III. Hydrological Linkages in Mesic and Arid Catchments -- IV. Conceptual Model -- V. Case Study: Sycamore Creek -- VI. Synthesis -- VII. Conclusions: Intermediate Disturbance and Nutrient Retention -- References. , Chapter 5. The Importance of Ground Water to Stream Ecosystem Function -- I. Introduction -- II. Influence of Ground Water on Stream Functioning -- III. Summary -- References -- Chapter 6. Surface-Subsurface Exchange and Nutrient Spiraling -- I. Introduction -- II. Empirical Studies -- III. A Stream Nutrient Spiraling Model with Subsurface Transient Storage -- IV. Results of Model Experiments -- V. Relevance of Model Experiments -- VI. Future Research Needs -- Reference -- Chapter 7. Emergent Biological Patterns and Surface-Subsurface Interactions at Landscape Scales -- I. Introduction -- II. The Balance of Physical and Chemical Factors on the Geologic Template and Emergent Biological Patterns -- III. Hydrothermal Systems as Models -- IV. Human Implants on Surface-Subsurface Interactions -- V. Synthesis and Recommendations for Future Studies -- References -- SECTION TWO: BIOGEOCHEMISTRY NUTRIENTS AND METABOLISM -- Chapter 8. Nitrogen Biogeochemistry and Surface-Subsurface Exchange in Streams -- I. Introduction -- II. Nitrogen Forms and Transformation Pathways in Fluvial Environments -- III. Nitrogen Sources in Fluvial Environments -- IV. Hydrologic Residence in Pristine Streams -- V. The Redox Environment -- VI. Ammonium Sorption to Hyporheic Sediments -- VII. Linking Nitrogen Transformation to Hydrologic Exchange in Hyporheic Zone Research -- VIII. What These Models Tell Us -- IX. Future Directions for Research -- References -- Chapter 9. Stream and Groundwater Influences on Phosphorus Biogeochemistry -- I. Introduction -- II. Sources and Forms of Phosphorus -- III. Abiotic Phosphorus Retention by Bed Sediments -- IV. Biotic Phosphorus Retention and Release within Bed Sediments -- V. Fluvial Dynamics and Physical Retention Mechanisms -- VI. Phosphorus and Surface-Subsurface Exchange: A Conceptual Model -- VII. Summary and Research Needs -- Reference. , Chapter 10. Surface and Subsurface Dissolved Organic Carbon -- I. Introduction -- II. DOC Concentrations -- III. Processes within the Hyporheic Zone -- References -- Chapter 11. Anoxia, Anaerobic Metabolism, and Biogeochemistry of the Stream-water-Groundwater Interface -- I. Introduction -- II. Methods Used in Studies of Anaerobic Metabolism -- III. Controls on the Establishment of Anoxia -- IV. Biogeochemistry and Evidence for Anaerobic Metabolism -- V. Influence of Subsurface Anaerobic Metabolism on Stream Ecosystem Processes -- VI. Conclusions and Future Research Directions -- Reference -- SECTION THREE: ORGANISMAL ECOLOGY -- Chapter 12. Microbial Communities in Hyporheic Sediments -- I. Introduction -- II. Physical and Chemical Environment -- III. The Organisms -- IV. Respiration -- V. Carbon Supply -- VI. Alternate Controls on Hyporheic Bacteria -- VII. Community Composition -- VIII. Conclusions and Research Needs -- References -- Chapter 13. The Ecology of Hyporheic Meiofauna -- I. Introduction -- II. Meiofaunal Taxa and Their Relative Abundance in the Hyporheic Zone -- III. Spatial Distribution and Abundance -- IV. Meiofauna and the Physical Environment -- V. Tolerance to Anoxia, Body Size, and Biomass -- VI. Trophic Roles, Dispersal Dynamics, and Response to Spatial-Temporal Heterogeneity -- VII. Meiofaunal-Microbial Interactions -- VIII. Meiofauna and Ecosystem Ecology -- IX. Conclusions and Future Research Needs -- References -- Chapter 14. The Subsurface Macrofauna -- I. Introduction -- II. Functional Classification of Subsurface Macrofauna -- III. Factors Influencing the Distribution of Subsurface Macrofauna -- IV. The Functional Role of Subsurface Macrofauna -- V. Potential Role as Biomonitors of Deteriorating Groundwater Quality -- VI. Conclusions -- Reference -- Chapter 15. Lotic Macrophytes and Surface-Subsurface Exchange Processes. , I. Introduction -- II. Macrophytes and Aquatic Habitats -- III. Macrophytes as Indicators of Surface and Subsurface Conditions -- IV. Macrophytes and Surface- and Subsurface Water Flow Patterns -- V. Nutrient Uptake from Sediments -- VI. Processes at the Rhizosphere -- VII. Summary and Avenues for Further Study -- Reference -- Chapter 16. Subsurface Influences on Surface Biology -- I. Introduction -- II. Effects on Primary Producers -- III. Effects on Microorganisms and Microbial Processes -- IV. Effects on Invertebrates -- V. Effects on Fish -- VI. Heterogeneity and Scale -- VII. Human Impacts -- VIII. Summary -- Reference -- SECTION FOUR: SUMMARYAND SYNTHESIS -- Chapter 17. Surface-Subsurface Interactions: Past, Present, and Future -- I. Introduction -- II. Growth and Development Trajectories -- III. Flowpaths and Interfaces -- IV. The Spatial Context -- V. Synthetic Models and Future Directions -- References -- Index.
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  • 2
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Stream ecology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (566 pages)
    Edition: 1st ed.
    ISBN: 9780124059191
    DDC: 577.64
    Language: English
    Note: Front Cover -- Stream Ecosystems in a Changing Environment -- Copyright -- Dedication -- Contents -- Contributors -- Acknowledgments -- Chapter 1: Hydrologic Exchange Flows and Their Ecological Consequences in River Corridors -- Introduction -- Origins of a Hydroecological Perspective in River Corridors -- Delineating Hydrologic Exchange Flows (HEFs) -- Ecological Relevance of HEFs -- Fluvial, Geomorphic, and Biological Influences on HEFs -- Physical Drivers of HEFs -- Hyporheic Exchange Flows -- Hydrologic Exchange with Off-Channel Surface Waters -- Bioroughness, Burrowing, and Bio-irrigation -- Temporally Dynamic HEFs -- Flood and ET-Driven Vertical Exchange with Streambed -- Bank Storage Exchange Flows -- River-Floodplain Exchanges -- Watershed Influences -- Understanding Controls and Predicting Consequences Across Scales -- Overview of Modeling Approaches -- Modeling Transport in River Corridors: From Spiraling to Transient Storage -- Water Mass Balance -- Combined Water and Chemical Mass Balance -- Reactive Chemical Transport -- The Spiraling Model -- Modeling Reactive Chemical Transport in Streams with Storage Zones -- Dynamic Reactive Transport Simulated by the Transient Storage Model -- Interpretation of HEF Parameters -- Prediction of HEFs Through Statistical Analysis of Published Data Sets -- Prediction of HEFs Using Physically Based Scaling Equations -- Hydrogeologic Modeling of HEFs -- Modeling Dynamic Exchanges with River Banks and Floodplains -- Incorporating the Multiple Scales of Exchange Flows in River Network Models -- Modeling Cumulative Effects of HEFs in River Networks -- Synthesis: From Challenges Emerge Opportunities -- Conclusions -- Topics to Stimulate Discussion -- References -- Chapter 2: Shaping the Physical Template: Biological, Hydrological, and Geomorphic Connections in Stream Channels -- Introduction. , Range of Variability in Alluvial Channels -- Disturbance-Recovery Regimes -- Water-Sediment-Morphology Interactions -- Vegetation Interactions -- Bio-Hydro-Geomorphic Templates for Stream Ecosystems -- Hydrogeomorphic Template for SW-GW Exchange -- Hydrogeomorphic Template for Light Availability -- Channel Complexity -- Geomorphic Considerations for Environmental Flows -- Geomorphically Effective Environmental Flows -- Environmental Flow Challenges in Intensively Altered River Systems -- Looking Forward and Downstream -- Are Rivers Just Large Streams? -- What Happens When Flow is No Longer Unidirectional? -- How Do Response Times in Stream Ecology Compare to Those in Fluvial Geomorphology? -- Which New Techniques and Technologies Will Allow Us to Answer the Above Questions? -- Discussion Questions -- Should We Restore Channel Complexity? -- How Do We Disentangle the Various Urban Influences on SW-GW Exchanges? -- What Would a Fluvial Geomorphic Model for Channel-Riparian Connections Look Like? -- References -- Chapter 3: Stream Microbial Ecology in a Changing Environment -- Introduction -- Changing Scientific Capacity -- Technological Advances -- Changing Template for SME -- Conclusions -- Future Directions -- Discussion Questions -- References -- Chapter 4: Metabolism of Streams and Rivers: Estimation, Controls, and Application -- Introduction -- Approaches to Measuring Reach-Scale Metabolism -- Balance and Coupling of GPP and ER in Streams -- Primary Controls on Metabolism -- Metabolic Control of Element Cycling in Streams -- From Human Effects on Metabolism to Application -- Looking Ahead -- Discussion Questions -- References -- Chapter 5: Nutrient Spiraling and Transport in Streams -- Introduction -- STOICMOD-A Stream Model Based on Spiraling and Ecological Stoichiometry -- Specific Fluxes -- Downstream Fluxes. , Lateral and Upstream Nutrient Input -- Allochthonous Input -- Leaf Decay by Miners -- Direct Mineralization -- Leaf Decay and Nutrient Uptake by Immobilizers -- Respiration and Indirect Mineralization -- Microbial Death -- Detritus and FBOM Entrainment and Algal Soughing -- Seston Entrainment and Deposition -- Primary Production and Algal Nutrient Uptake -- Algal Mineralization -- Model Parameterization and Programming -- Simulations -- Simulations With Autotrophic Model Components Only -- Simulations With Heterotrophic Model Components Only -- Simulations With Both Autochthonous and Allochthonous Energy Inputs -- Climate Change Experiments -- Results of Elevated Temperature -- Response to Elevated Dissolved Nutrients -- Conclusions -- Discussion Questions -- References -- Chapter 6: Dissolved Organic Matter in Stream Ecosystems: Forms, Functions, and Fluxes of Watershed Tea -- Introduction -- DOM Sources -- Autochthonous Inputs -- Allochthonous Inputs -- Hydrologic Connections -- The Impact of Landscapes and Topography -- Molecular Characterization of DOM -- Quantitative Geochemistry -- Optical Methods -- DOM Composition and Structure -- DOM Chemogeography and Chemodiversity -- DOM Transformations and Fates -- Oxidative Reactivity of DOM -- Bio-Reactivity of DOM -- Conceptual Models of DOM Diagenesis and Substances -- Pathways and Products of Photooxidation -- Interactions Between Photochemistry and Biological Degradation -- Rates of Photooxidation in Waters -- DOM Contributions to Ecosystem Metabolism -- DOM Uptake -- Instream Hydrologic Forcing and DOM Export -- DOM in the Anthropocene -- Altering Ecosystems -- Urbanization -- Impacts of a Changing Environment -- Summary of Impacts of the Anthropocene on DOM Sources and Processing -- Future Research Challenges -- Discussion Topics -- Acknowledgments -- References. , Chapter 7: Stream-Lake Interaction: Understanding Coupled Hydro-Ecological Systems -- Introduction -- Conceptual Frameworks in Stream and Lake Ecology -- The Physical Template of Coupled Stream-Lake Systems -- Implications of Stream-Lake Interactions for Nutrient Spiraling -- Effects of Stream-Lake Interaction on Benthic Invertebrates and Fishes -- Stream-Lake Interactions in a Changing Environment and Future Directions -- Discussion Questions -- References -- Chapter 8: From Headwaters to Rivers to River Networks: Scaling in Stream Ecology -- Introduction -- Problem Addressed in This Chapter/Objectives -- Scaling Defined -- Mathematical Framework -- Scaling Physical Characteristics -- Scaling Chemical Characteristics: The Terrestrial-Aquatic Linkage -- Scaling Biological Characteristics -- Type of Reaction Rate for Broad Scale Modeling -- Reaction Rate Kinetics -- Controls of Reaction Rate Parameters -- New Sources and Coupled Processes -- Scaling Heterogeneity and Connectivity -- Aquatic Ecosystem Heterogeneity and Connectivity in the River Network -- Impacts of a Changing Environment -- Supply -- Discharge -- Concentrations -- Connectivity ( α) -- Demand -- Width, Length, and A s / A -- Uptake -- Forward Looking -- Opportunities -- Hypotheses of Changing Role of River Network in a Changing Environment -- Challenges -- Discussion Topics -- Acknowledgments -- References -- Chapter 9: Landscape and Regional Stream Ecology -- Introduction -- Historic Context -- Streams as Landscapes -- Gradients and Streams -- Patches and Hierarchies and Streams -- Issues of Scale -- Patch Size, Shape, Composition, Configuration, and Connectivity -- Final Comments on Streams as Landscapes -- Streams in Landscapes -- Streams Across Landscapes -- Regional Frameworks -- Cross-Site Studies -- Conclusion -- Discussion Topics -- References. , Chapter 10: Global Models of River Biogeochemical Functioning -- Introduction -- Challenges in Examining Current and Future Material Fate and Transport Across Regions and Continents -- River Geomorphic Template -- Hydrologic Stationarity -- Land Use Change -- Climate Departure From Normal Conditions to Extremes -- Modeling Approaches and Limitations to Quantifying River Processing and Export Across Regions -- Introduction -- Biogeochemical Simulations in Current Watershed Models -- Hyporheic and Shallow Subsurface Flow -- River-Floodplain Connectivity -- Process-Based Nutrient Cycling and Sediment Transport Models -- Process-Based Nitrogen Cycling and Ecological Stoichiometry -- Recent Progress in Integrative Models -- Summarizing the Challenges -- Final Thoughts -- Future Generation of Models -- Thought Activities and Discussion -- References -- Chapter 11: Human Impacts on Stream Hydrology and Water Quality -- Introduction -- Human Impacts on Stream Environments -- Modes of Modification of the Landscape by Humans -- Physical Modifications -- Changing Soil Surfaces -- Rates of Erosion -- Enhanced Drainage -- Channel Modifications -- Ecological Modification -- Interception -- Transpiration -- Grazing -- Biogeochemical Modifications -- Fertilizers -- Pesticides -- Impacts of Landscape Modifications on the Stream Environment -- Hydrological Impacts -- Physical Impacts -- Water Quality -- Temperature -- Nutrients -- Pesticides -- Habitat and Biodiversity -- Unifying Themes Across Intensively Managed Landscapes -- The "Homogenization" Hypothesis -- Landscape Homogenization -- Homogenization of Hydrologic Response -- Agricultural Streams -- Urban Streams -- Homogenization of Biogeochemical Responses -- Ecological Homogenization -- Time Lags and Legacy -- Physical Legacy -- Nutrient Legacies and Time Lags -- Hydrologic Time Lag. , Biogeochemical Legacy and Time Lag.
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford UK : Blackwell Science Ltd
    Freshwater biology 47 (2002), S. 0 
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: 1. Groundwater fluxes of nitrogen and dissolved organic carbon (DOC) were investigated in Grape Vine Canyon Stream in the Mojave Desert focusing on the rate of inputs and the fate of groundwater-derived nutrients in the stream. Discharge rates from different ground waters were measured using an end-member mixing model coupled with injections of a conservative solute tracer into the stream channel.2. In surface water, nitrate concentration averaged 1.13 mg N L–1 and DOC concentration averaged 1.82 mg C L–1.3. Groundwater discharge into Grape Vine Canyon Stream was derived from three sources. Nitrate concentration varied among the three groundwater sources with mean concentrations of 0.56, 0.94 and 0.08 mg N L–1. DOC, in contrast, did not vary among ground water sources, with an overall average concentration of 2.96 mg C L–1.4. In the surface stream, nitrate concentration was two-fold greater than the concentration predicted from groundwater input, indicating that in-stream processes generated nitrate. Stream DOC concentration was lower than predicted based upon groundwater input rate. The production of nitrate and loss of DOC suggest that DOC is lost through mineralisation of dissolved organic matter, possibly resulting in the mineralisation of dissolved organic nitrogen to ammonium and subsequent transformation to nitrate via nitrification. In further support of this hypothesised linkage, DOC loss explained 80–89% of the variance in nitrate production in Grape Vine Canyon Stream.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Titan, Saturn's largest moon, is the only Solar System planetary body other than Earth with a thick nitrogen atmosphere. The Voyager spacecraft confirmed that methane was the second-most abundant atmospheric constituent in Titan's atmosphere, and revealed a rich organic chemistry, but its ...
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1573-5117
    Keywords: dissolved organic carbon ; organic matter export ; desert streams
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Dissolved organic carbon (DOC) dynamics were examined over five years (1989–1993) in Sycamore Creek, a Sonoran Desert stream, specifically focusing on DOC concentration in surface and hyporheic waters, and rates of export. In 1989 and 1990, the years of lowest stream discharge (0.08 and 0.04 m3 s−1 annual mean of daily discharge, respectively), DOC was high, averaging 7.37 and 6.22 mgC l−1 (weighted annual means). In contrast, from 1991 through 1993, a period of increased flow (1.1, 1.2 and 4.3 m3 s−1), concentration was significantly lower (P〈0.001) with annual mean concentrations of 3.54, 3.49 and 3.39 mgC l−1. Concentration exhibited little spatial variation between two sampling stations located 6 km apart along the mainstem or between surface and hyporheic waters. Annual export of DOC from Sycamore Creek varied 100-fold over the five-year period from a mean rate of only 24 kgC d−1 in 1990 to 2100 kgC d−1 in 1993. Ninety percent of DOC was exported by flows greater than 2.8 m3 s−1, and 50% during flows greater than 27 m3 s−1; flows of 2.8 and 24 m3 s−1 occurred only 9 and 1% of the time. The export of organic matter in Sycamore Creek appears to be coupled to El Niño-Southern Oscillation phenomena. The years of highest export, 1991–1993, had El Niño conditions while 1989 and 1990 had medial conditions.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 33 (1996), S. 125-146 
    ISSN: 1573-515X
    Keywords: Denitrification ; stream ecology ; nutrient dynamics ; nitrification ; hyporheic zone ; parafluvial zone
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract Denitrification was measured in hyporheic, parafluvial, and bank sediments of Sycamore Creek, Arizona, a nitrogen-limited Sonoran Desert stream. We used three variations of the acetylene block technique to estimate denitrification rates, and compared these estimates to rates of nitrate production through nitrification. Subsurface sediments of Sycamore Creek are typically well-oxygenated, relatively low in nitrate, and low in organic carbon, and therefore are seemingly unlikely sites of denitrification. However, we found that denitrification potential (C & N amended, anaerobic incubations) was substantial, and even by our conservative estimates (unamended, oxic incubations and field chamber nitrous oxide accumulation), denitrification consumed 5–40% of nitrate produced by nitrification. We expected that denitrification would increase along hyporheic and parafluvial flowpaths as dissolved oxygen declined and nitrate increased. To the contrary, we found that denitrification was generally highest at the upstream ends of subsurface flowpaths where surface water had just entered the subsurface zone. This suggests that denitrifiers may be dependent on the import of surface-derived organic matter, resulting in highest denitrification rate at locations of surface-subsurface hydrologic exchange. Laboratory experiments showed that denitrification in Sycamore Creek sediments was primarily nitrogen limited and secondarily carbon limited, and was temperature dependent. Overall, the quantity of nitrate removed from the Sycamore Creek ecosystem via denitrification is significant given the nitrogen-limited status of this stream.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1573-515X
    Keywords: carbon dioxide ; eastern Tennessee ; ecosystem metabolism ; methane ; streams ; Smoky Mountains
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract The partial pressures of CO2 (pCO2) andCH4 (pCH4) in streams are not only governed byinstream processes, but also by transformations occurring in soil andgroundwater ecosystems. As such, stream water pCO2 andpCH4 can provide a tool to assess ecosystem respiration andanaerobic metabolism throughout drainage basins. We conducted three surveyssampling the gas content of streams in eastern Tennessee and western NorthCarolina to assess factors regulating ecosystem metabolism in catchmentswith contrasting geomorphologies, elevations and soil organic matterstorage. In our first survey, the influence of drainage basin geomorphologyon ecosystem respiration was examined by sampling streams drainingcatchments underlain by either shale or dolomite. Geomorphology isinfluenced by geology with shale catchments having shallower soils, broader,unconstrained valley floors compared with dolomite catchments.pCO2 varied little between catchment types but increased froman average of 3340 ppmv in spring to 9927 ppmv in summer or 9.3 and 28 timesatmospheric equilibrium (pCO2(equilib)), respectively. Incontrast, pCH4 was over twice as high in streams drainingshale catchments (306 ppmv; pCH4(equilib) = 116) compared withmore steeply incised dolomite basins (130 ppmv; pCH4(equilib)= 51). Using the ratio of pCH4:pCO2 as an indexof anaerobic metabolism, shale catchments had nearly twice as muchanaerobiosis (pCH4:pCO2 = 0.046) than dolomitedrainages (pCH4:pCO2 = 0.024). In our secondsurvey, streams were sampled along an elevational gradient (525 to 1700 m)in the Great Smoky Mountains National Park, USA where soil organic matterstorage increases with elevation. pCO2 did not vary betweenstreams but increased from 5340 ppmv (pCO2(equilib) = 15) to8565 ppmv (pCO2(equilib) = 24) from spring to summer,respectively. During spring pCH4 was low and constant acrossstreams, but during summer increased with elevation ranging from 17 to 2068ppmv (pCH4(equilib) = 10 to 1216). The contribution ofanaerobiosis to total respiration was constant during spring(pCH4:pCO2 = 0.017) but during summer increasedwith elevation from 0.002 at 524 m to 0.289 at 1286 m. In our last survey,we examined how pCO2 and pCH4 changed withcatchment size along two rivers (ca. 60 km stretches in both riverscorresponding to increases in basin size from 1.7–477km2 and 2.5–275 km2). pCO2and pCH4 showed opposite trends, with pCO2decreasing ca. 50% along the rivers, whereas pCH4roughly doubled in concentration downstream. These opposing shifts resultedin a nearly five-fold increase of pCH4:pCO2along the rivers from a low of 0.012 in headwaters to a high of 0.266 65-kmdownstream. pCO2 likely declines moving downstream asgroundwater influences on stream chemistry decreases, whereaspCH4 may increase as the prevalence of anoxia in riversexpands due to finer-grained sediments and reduced hydrologic exchange withoxygenated surface water.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 31 (1995), S. 155-173 
    ISSN: 1573-515X
    Keywords: methane ; methanogenesis ; arid-lands ; Sonoran Desert ; streams ; hydrologic exchange
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract Methanogenesis was studied in five streams of central and southern Arizona by examining the distribution of methane in interstitial water and evasion of methane in three subsystems (hyporheic, parafluvial and bank sediments). In Sycamore Creek, the primary study site (studied during summer and early autumn), methane content of interstitial water exhibited a distinct spatial pattern. In hyporheic (sediments beneath the wetted channel) and parfluvial zones (active channel sediments lateral to the wetted channel), which were well oxygenated due to high hydrologic exchange with the surface stream and had little particulate organic matter (POM), interstitial methane concentration averaged only 0.03 mgCH4-C/L. Bank sediments (interface between the active channel and riparian zone), in contrast, which were typically vegetated, had high POM, low hydrologic exchange and concomitantly low dissolved oxygen levels, had interstitial concentration averaging 1.5 mgCH4-C/L. Methane emission from Sycamore Creek, similar to methane concentration, averaged only 3.7 mgCH4-C·m−2·d−1 from hyporheic and parafluvial zones as opposed to 170 mgCH4-C·m−2·d−1 from anoxic bank sediments. Methane in four additional streams sampled (one sampling date during late winter) was low and exhibited little spatial variation most likely due to cooler stream temperatures. Interstitial methane in parafluvial and bank sediments of all four streams ranged from only 0.005 to 0.1 mgCH4-C/L. Similarly methane evasion was also low from these streams varying from 0 to 5.7 mgCH4-C·m−2·d−1. The effects of organic matter and temperature on methanogenesis were further examined by experimentally manipulating POM and temperature in stoppered flasks filled with hyporheic sediments and stream water. Methane production significantly increased with all independent variables. Methane production is greatest in bank sediments that are relatively isolated hydrologically and lowest in hyporheic and parafluvial sediments that are interactive with the surface stream.
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  • 9
    Publication Date: 2017-06-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 10
    Publication Date: 2022-05-26
    Description: © The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Environmental Research Letters 11 (2016): 034014, doi:10.1088/1748-9326/11/3/034014.
    Description: As the permafrost region warms, its large organic carbon pool will be increasingly vulnerable to decomposition, combustion, and hydrologic export. Models predict that some portion of this release will be offset by increased production of Arctic and boreal biomass; however, the lack of robust estimates of net carbon balance increases the risk of further overshooting international emissions targets. Precise empirical or model-based assessments of the critical factors driving carbon balance are unlikely in the near future, so to address this gap, we present estimates from 98 permafrost-region experts of the response of biomass, wildfire, and hydrologic carbon flux to climate change. Results suggest that contrary to model projections, total permafrost-region biomass could decrease due to water stress and disturbance, factors that are not adequately incorporated in current models. Assessments indicate that end-of-the-century organic carbon release from Arctic rivers and collapsing coastlines could increase by 75% while carbon loss via burning could increase four-fold. Experts identified water balance, shifts in vegetation community, and permafrost degradation as the key sources of uncertainty in predicting future system response. In combination with previous findings, results suggest the permafrost region will become a carbon source to the atmosphere by 2100 regardless of warming scenario but that 65%–85% of permafrost carbon release can still be avoided if human emissions are actively reduced.
    Description: This work was supported by the National Science Foundation ARCSS program and Vulnerability of Permafrost Carbon Research Coordination Network (grants OPP-0806465, OPP-0806394, and 955713) with additional funding from SITES (Swedish Science Foundation), Future Forest (Mistra), and a Marie Curie International Reintegration Grant (TOMCAR-Permafrost #277059) within the 7th European Community Framework Programme.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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