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  • 1
    Online Resource
    Online Resource
    New York :Cambridge University Press,
    Keywords: Estuarine ecology. ; Electronic books.
    Description / Table of Contents: A comprehensive, state-of-the-art synthesis of biogeochemical dynamics at major river-coastal interfaces for advanced students and researchers. It presents a unique perspective on how humans have altered these systems, as well as the implications of these changes on issues as diverse as the health of fisheries and the global carbon budget.
    Type of Medium: Online Resource
    Pages: 1 online resource (674 pages)
    Edition: 1st ed.
    ISBN: 9781107503571
    DDC: 577.14
    Language: English
    Note: Intro -- Contents -- List of Contributors -- Preface -- Section I Introduction -- 1 An introduction to the biogeochemistry of river-coastal systems -- 1. Introduction -- 2. Riverine inputs of particulate and dissolved organic matter to the coastal ocean -- 2.1. The conundrum of missing OC -- 3. Transport processes and controls on OM preservation -- 4. CO2 fluxes in coastal waters -- 5. Possible links between coastal water CO2 flux and riverine loadings -- 6. Directions for future research -- Section II Water and sediment dynamics from source to sink -- 2 Water and sediment dynamics through the wetlands and coastal water bodies of large river deltaic plains -- 1. Introduction -- 2. Mechanisms of water and sediment input to the delta plain -- 2.1. Avulsion and distributary channel evolution -- 2.2. Overbank and crevasse processes -- 2.3. Groundwater and rainwater input -- 3. Processes and simulation of water and sediment circulation in deltaic plains and estuaries -- 3.1. Controlling physical processes -- 3.2. Simulation of water and sediment processes -- 3.3. Numerical modeling tools -- 4. The role of wetlands -- 4.1. Introduction to the ecogeomorphology of deltaic plain wetlands -- 4.2. Controls on deltaic wetland development -- 4.3. Large river wetlands as particle sources, sinks, and loci of particle transformation -- 5. Conclusions -- 3 Freshwater and sediment dispersal in large river plumes -- 1. Introduction -- 2. The anatomy of a river plume -- 2.1. Salinity space -- 2.2. The estuary -- 2.3. The near-field plume -- 2.4. The mid-field plume, or the bulge -- 2.5. Far-field plume -- 2.6. Very far-field plume -- 3. River plume classification -- 4. Sediment dispersal -- 4.1. Sediment dynamics -- 4.1.1. Buoyancy effect -- 4.1.2. Flocculation and hindered settling -- 4.2. Riverine input and carrying capacity. , 4.3. The near-, mid-, and far-field dispersal -- 5. Concluding remarks -- 4 Shelf and slope sedimentation associated with large deltaic systems -- 1. Introduction -- 2. Overview of large deltaic systems -- 3. Amazon: a subaqueous delta clinoform system -- 4. Ganges-Brahmaputra: a combination of influences -- 5. Mississippi-Atchafalaya: a proximal accumulation-dominated system -- 6. Fluvial and marine controls on large deltaic systems -- 7. Geological framework and human influence on large deltaic systems -- 8. Conclusions -- Acknowledgments -- 5 Changjiang (Yangtze) and Huanghe (Yellow) Rivers: historical reconstruction of land-use change and sediment load to the sea -- 1. Regional settings of the Changjiang and Huanghe River basins -- 1.1. Topographic settings -- 1.2. Hydrologic settings -- 1.3. Surface lithology of the river basins -- 2. Human impacts on the river basins and land-use change -- 3. Anthropogenic alteration of the rivers since the 1950s -- 3.1. Variation of the Changjiang sediment flux since the 1950s -- 3.2. Variation of the Huanghe sediment flux since the 1950s -- 4. Roles of climate change and human activities on river systems -- 5. The future of the mega-deltas of Changjiang and Huanghe -- 6. Conclusion -- 6 Flux and fate of the Yellow (Huanghe) River-derived materials to the sea: impacts of climate change and human activities -- 1. Introduction -- 2. Historical changes of the Yellow River water and sediment discharge -- 2.1. Sediment fluxes on the millennial scale -- 2.2. Sediment fluxes on the decadal scale -- 2.3. Causes of the recent decrease of the water and sediment discharge -- 2.4. Impacts of the recent-year water discharges and sediment loads decreasing -- 3. Fate of yellow river sediments in the Bohai and Yellow Seas -- 3.1. Rapid accumulations near the river mouth: proximal deltaic depocenter. , 3.2. Longshore transport to the Yellow Sea: distal mud depocenter -- 4. Conclusions -- 7 Carbon dioxide dynamics and fluxes in coastal waters influenced by river plumes -- 1. Introduction -- 2. CO2 degassing flux in inner estuaries -- 3. Distribution pattern of pCO2 in river plumes and control mechanisms -- 3.1. River carbonate contents and the associated buffering capacity changes during river-ocean mixing -- 3.2. CO2 in the Changjiang River plume -- 3.3. CO2 in the Mississippi River plume -- 3.4. CO2 in the Amazon River plume -- 4. A tentative estimate of global river-plume CO2 flux -- Acknowledgment -- 8 Impacts of watershed processes on exported riverine organic carbon -- 1. Introduction -- 2. POC Sources -- 2.1. Vegetation -- 2.2. Soils -- 2.3. The deeper regolith and geomorphic processes -- 2.4. In-channel and lowland sources and processes -- 3. Climate impacts on riverine OC -- 4. Predicting the exported riverine organic signature -- 5. Summary -- Acknowledgments -- 9 Black carbon in coastal and large river systems -- 1. Introduction -- 2. Sources of black carbon -- 2.1. Atmospheric BC -- 2.2. Soil BC -- 2.3. Dissolved BC -- 3. Isolation, quantification, and source discrimination methods for black carbon -- 3.1. Visual methods for BC quantification -- 3.2. Chemical and thermal BC quantification methods -- 3.3. Isolation of BC in the dissolved phase -- 3.4. Source discrimination of BC -- 4. Black carbon in large river systems -- 4.1. Fluvial BC -- 4.2. Global pyrogenic PAH discharge and comparison with BC -- 5. Fate of black carbon -- 5.1. Storage BC in the ocean -- 5.2. Degradation of BC -- 6. Conclusions -- Section III Eastern hemisphere systems -- 10 Carbon biogeochemistry in the continuum of the Changjiang (Yangtze) River watersheds across the East China Sea -- 1. Introduction. , 2. Characters of the land-source influx and open boundary processes -- 2.1. Dissolved inorganic carbon and CH4 -- 2.2. Dissolved organic carbon and particulate organic carbon -- 2.3. Pigments -- 3. Major pathways of carbon cycle and influence factors -- 3.1. DIC and CH4 -- 3.2. DOC and POC -- 3.3. Carbon fate inferred from pigments -- 4. Biogeochemical budgets and feedbacks to open ocean and atmosphere -- 5. Evidence of historical records -- 6. Biogeochemical provinces of the Changjiang estuary - ECS in the perspective of carbon biogeochemistry -- 7. Concluding remarks and future work -- Acknowledgments -- 11 Dynamics of phytoplankton blooms and nutrient limitation in the Pearl River (Zhujiang) estuarine coastal waters -- 1. Introduction -- 2. General geographic and oceanographic settings of the Pearl River estuary -- 3. Processes in estuarine and coastal waters -- 4. Spatial and seasonal variability of phytoplankton biomass -- 4.1. River outflow controlled variability -- 4.2. Tidal cycle regulated variability -- 4.3. Wind event driven variability -- 5. Dynamics of nutrients and nutrient limitation variability -- 6. Potential effects of climate change on eutrophication -- 7. Conclusions -- Acknowledgments -- 12 The Mekong River and its influence on the nutrient chemistry and matter cycling in the Vietnamese coastal zone -- 1. Introduction -- 2. Climatology of the Southeast Asian monsoon region -- 3. Hydrography of the Vietnamese coastal waters -- 4. The Mekong River and river plume -- 5. Biochemistry and productivity in the Mekong plume and coastal waters -- 5.1. Phytoplankton species composition -- 5.2. Primary production and nitrogen fixation -- 5.3. Food web and zooplankton nutrition -- 6. How does this compare with other tropical estuaries? -- 7. Future of the Mekong estuary and its catchment -- 8. Conclusion -- Acknowledgment. , 13 Physical dynamics and biogeochemistry of the Pearl River plume -- 1. Introduction -- 2. Basics of the Pearl River, estuary, and the shelf -- 2.1. The Pearl River -- 2.1.1. Basics -- 2.1.2. Precipitation and river discharge -- 2.2. Pearl River estuary -- 2.2.1. Basics -- 2.2.2. Circulation in the estuary -- 2.2.2.1. Gravitational circulation -- 2.2.2.2. Subtidal circulation -- 2.2.2.3. Intra-tidal circulation -- 2.2.3. Hydrology and biogeochemistry of the PRE -- 2.2.4. Conceptual summary and about the mixing behavior: Conservative and nonconservative -- 2.3. Northern South China Sea Shelf -- 2.3.1. Basics -- 2.3.2. Shelf circulation in the northern South China Sea -- 2.3.2.1. Upwelling circulation in summer (wet season) -- 2.3.2.2. Downwelling circulation in winter (dry season) -- 3. Physical dynamics and biogeochemistry of the plume -- 3.1. Plume over the Shelf -- 3.2. Plume effect on the shelf circulation -- 3.3. Biogeochemistry of the river plumes -- 3.3.1. Case of May 2001 -- 3.3.2. Case of August 2008 -- 3.3.3. Comparison between 2001 and 2008 -- 4. Coupling the physical dynamics and biogeochemistry -- 4.1. Mixing of different water masses -- 4.2. Coupled physical-biogeochemical model -- 5. Summary and perspectives -- Acknowledgment -- 14 The evolution of carbon signatures carried by the Ganges-Brahmaputra river system: a source-to-sink perspective -- 1. Introduction to the Ganges-Brahmaputra river system -- 2. Reworking and deposition of fluvial sediment and organic carbon in the Bay of Bengal -- 3. Characterization of organic carbon signatures of the Ganges and Brahmaputra rivers and the Bengal Fan -- 4. Carbon sources, transformations, and storage in the Himalayan range -- 5. Carbon sources, transformations, and storage in the Ganges floodplain -- 6. Carbon sources, transformations, and storage in the Brahmaputra floodplain. , 7. Carbon export from the G-B basin to the Bengal Fan.
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  • 2
    Keywords: Regression analysis. ; Electronic books.
    Description / Table of Contents: Written in simple language with relevant examples, this illustrative introductory book presents best practices in experimental design and simple data analysis. Taking a practical and intuitive approach, it only uses mathematical formulae to formalize the methods where necessary and appropriate. The text features extended discussions of examples that include real data sets arising from research. The authors analyze data in detail to illustrate the use of basic formulae for simple examples while using the GenStat statistical package for more complex examples. Each chapter offers instructions on how to obtain the example analyses in GenStat and R.
    Type of Medium: Online Resource
    Pages: 1 online resource (592 pages)
    Edition: 1st ed.
    ISBN: 9781439898055
    DDC: 570.1/5195;570.15195
    Language: English
    Note: Front Cover -- Contents -- Preface -- Authors -- Chapter 1: Introduction -- Chapter 2: A Review of Basic Statistics -- Chapter 3: Principles for Designing Experiments -- Chapter 4: Models for a Single Factor -- Chapter 5: Checking Model Assumptions -- Chapter 6: Transformations of the Response -- Chapter 7: Models with a Simple Blocking Structure -- Chapter 8: Extracting Information about Treatments -- Chapter 9: Models with More Complex Blocking Structure -- Chapter 10: Replication and Power -- Chapter 11: Dealing with Non-Orthogonality -- Chapter 12: Models for a Single Variate: Simple Linear Regression -- Chapter 13: Checking Model Fit -- Chapter 14: Models for Several Variates: Multiple Linear Regression -- Chapter 15: Models for Variates and Factors -- Chapter 16: Incorporating Structure: Linear Mixed Models -- Chapter 17: Models for Curved Relationships -- Chapter 18: Models for Non-Normal Responses: Generalized Linear Models -- Chapter 19: Practical Design and Data Analysis for Real Studies -- References -- Appendix A: Data Tables -- Appendix B: Quantiles of Statistical Distributions -- Appendix C: Statistical and Mathematical Results -- Back Cover.
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  • 3
    Publication Date: 2022-05-25
    Description: This paper is not subject to U.S. copyright. The definitive version was published in Palaeogeography, Palaeoclimatology, Palaeoecology 246 (2007): 120-136, doi:10.1016/j.palaeo.2006.10.030.
    Description: The Hudson Shelf Valley (HSV) is the largest physiographic feature on the U.S. mid-Atlantic continental shelf. The 150-km long valley is the submerged extension of the ancestral Hudson River Valley that connects to the Hudson Canyon. Unlike other incised valleys on the mid-Atlantic shelf, it has not been infilled with sediment during the Holocene. Analyses of multibeam bathymetry, acoustic backscatter intensity, and high-resolution seismic reflection profiles reveal morphologic and stratigraphic evidence for a catastrophic meltwater flood event that formed the modern HSV. The valley and its distal deposits record a discrete flood event that carved 15-m high banks, formed a 120-km2 field of 3- to 6-m high bedforms, and deposited a subaqueous delta on the outer shelf. The HSV is inferred to have been carved initially by precipitation and meltwater runoff during the advance of the Laurentide Ice Sheet, and later by the drainage of early proglacial lakes through stable spillways. A flood resulting from the failure of the terminal moraine dam at the Narrows between Staten Island and Long Island, New York, allowed glacial lakes in the Hudson and Ontario basins to drain across the continental shelf. Water level changes in the Hudson River basin associated with the catastrophic drainage of glacial lakes Iroquois, Vermont, and Albany around 11,450 14C year BP (~ 13,350 cal BP) may have precipitated dam failure at the Narrows. This 3200 km3 discharge of freshwater entered the North Atlantic proximal to the Gulf Stream and may have affected thermohaline circulation at the onset of the Intra-Allerød Cold Period. Based on bedform characteristics and fluvial morphology in the HSV, the maximum freshwater flux during the flood event is estimated to be ~ 0.46 Sv for a duration of ~ 80 days.
    Description: Support for N. Driscoll was provided by the Office of Naval Research and the National Science Foundation
    Keywords: Continental shelf ; Glacial lakes ; Meltwater ; Sea-level rise ; Transgression ; Wisconsinan
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © Oceanography Society, 2017. This article is posted here by permission of Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 30, no. 3 (2017): 22–33, doi:10.5670/oceanog.2017.311.
    Description: Significant sediment transformation and trapping occur along the tidal and estuarine reaches of large rivers, complicating sediment source signals transmitted to the coastal ocean. The collaborative Mekong Tropical Delta Study explored the tidally influenced portion of the Mekong River to investigate processes that impact mud- and sand-sized sediment transport and deposition associated with varying fluvial and marine influences. Researchers participating in this 2014–2015 project found that as sand and mud progress down the tidal portion of the river, sands in suspension can settle during reduced or slack flows as river discharge becomes progressively more affected by tides in the seaward direction. Consequently, deposits on the tidal river bed are connected to sand transport in the channel. In contrast, fine mud particles remain in suspension until they reach an interface zone where waters are still fresh, but the downstream saline estuary nonetheless impacts the flows. In this interface zone, as within the estuary, fine particles tend to settle, draping the sand beds with mud and limiting the connection between the bed and suspended sand. In the Mekong system, the interface and estuarine zones migrate along the distributary channels seasonally, resulting in variable trapping dynamics and channel bed texture. Therefore, the signature of fluvial-sediment discharge is altered on its path to the coastal ocean, and the disconnected mud and sand supply functions at the river mouth should result in distinct offshore depositional signatures.
    Description: This research was funded by the US Office of Naval Research (grant numbers: N00014-15-1-2011, N00014- 13-1-0127, N00014-13-1-0781, N00014-14-1-0145).
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 5
    ISSN: 1365-3180
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: The algorithm of an optical detection system was first investigated for its ability to correctly classify transplanted crops and weeds during the critical early stages of crop establishment and its robustness over a range of different crop species. The trade-off was then examined between increasing the sensitivity of the detection system vs. the possibility of, in doing so, misclassifying some crop plants as weeds and inadvertently removing them. This was achieved by running a competition model using parameters derived from the image analysis and assessing the outcome of scenarios in terms of yield. The optimum parameter values to maximize the detection of the crop and the optimum parameter values to maximize the detection of the weed appeared relatively insensitive to time of image capture or weed density. They also appeared insensitive for different crop species where the crop had similar growth habit. However, competition scenarios indicated that the detection system parameter settings to achieve optimum yields were sensitive to the competitive ability of the weed species. For Veronica persica, crop yield was more sensitive to accidental crop removal than from competition. In contrast, in the presence of Tripleurospermum inodorum, yield loss was more attributable to weed competition. Importantly, linking the detection system with the competition model illustrated the principle that optimum yield may not necessarily be obtained by maximizing weed removal or minimizing crop removal. This first example of combining a detection system with a competition model presents a new opportunity to quantify the sensitivity of image classification in terms of yield.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Weed research 44 (2004), S. 0 
    ISSN: 1365-3180
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Total weed control within a crop is both difficult and expensive to achieve, so that some weeds will often remain to set seed. The seed production resulting from these weeds will ultimately affect the sustainability of the weed control strategy. If too much is allowed to return each season there could be a gradual, but significant, increase in the potential weed flora over a number of seasons. Field trials were carried out in 2000 and 2001 to quantify the potential magnitude of this weed seed return from Chenopodium album L., grown at two planting densities either in pure stands or in competition with one of two crops (cabbage or onion). Crop and weed weights and weed seed production were notably greater in 2001. Both dry weight and seed production of C. album were suppressed by increasing planting density or by the presence of crop, with cabbage having a more suppressive effect. Despite the plasticity in seed production, a linear relationship was demonstrated between log weed seed production and log weed biomass that was robust over a range of competitive situations with onion and cabbage, at different planting densities and in growing seasons. The study also demonstrated that the relationship could be combined with an existing simple competition model to allow the consequences of incomplete weed control to be assessed in terms of potential weed seed return.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Weed research 36 (1996), S. 0 
    ISSN: 1365-3180
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Experiments to monitor weed seedling emergence from various soil depths were begun in 1989. Recently shed seeds were buried in either narrow bands at a range of depths in the soil or mixed evenly between the soil surface and each of these depths. Total emergence of Stellaria media (L.) Vill., Matricaria spp., Veronica persica Poiret, Veronica arvensis L. and Polygonum aviculare L., declined with increasing depth of burial. A similar pattern was observed for Chenopodium album L. with the exception of emergence from the surface layer. The reduction in emergence with increasing soil depth was greater for seeds in the narrow-banded treatments than for those in broad layers. A model was developed using the data from the narrow-banded treatments to predict emergence from distributions over broad layers. Predictions from the model closely agree with the data from the present broad-layer treatments and those from a similar experiment made in the 1960s. By including the effects of depth of seed burial on seedling emergence, this model could be combined with models that determine the effects of cultivation on seed distribution, and therefore improve precision of predictions of seedling emergence from the seedbank.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Plant pathology 40 (1991), S. 0 
    ISSN: 1365-3059
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1365-3180
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary The emergence behaviour of weed species in relation to cultural and meteorological events was studied. Dissimilarities between populations in dormancy and germination ecology, between-year maturation conditions and seed quality and burial site climate all contribute to potentially unpredictable variability. Therefore, a weed emergence data set was produced for weed seeds of Stellaria media and Chenopodium album matured and collected from three populations (Italy, Sweden and UK). The seeds were collected in two consecutive seasons (1999 and 2000) and subsequently buried in the autumn of the same year of maturation in eight contrasting climatic locations throughout Europe and the USA. The experiment sought to explore and explain differences between the three populations in their emergence behaviour. Evidence was demonstrated of synchrony in the timing of the emergence of different populations of a species at a given burial site. The relative magnitudes of emergence from the three populations at a given burial site in a given year were generally similar across all the burial sites in the study. The resulting data set was also used to construct a simple weed emergence model, which was tested for its application to the range of different burial environments and populations. The study demonstrated the possibility of using a simple thermal time-based model to describe part of the emergence behaviour across different burial sites, seed populations and seasons, and a simple winter chilling relationship to adjust for the magnitude of the flush of emergence at a given burial site. This study demonstrates the possibility of developing robust generic models for simple predictions of emergence timing across populations.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1365-3059
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Laboratory assays demonstrated that two isolates of Trichoderma viride and one isolate of Trichoderma pseudokoningii degraded up to 80% of sclerotia of four isolates of Sclerotium cepivorum in a silty clay soil, and also degraded up to 60% of sclerotia in three other soil types. Relationships were defined between the degree of sclerotial degradation by the two T. viride isolates in the silty clay soil and both temperature and soil water potential. Sclerotia were degraded between 10 and 25°C at −0·00012 MPa, but there was little activity of T. viride at 5°C or at −4 MPa. Degradation of S. cepivorum sclerotia also occurred in the absence of Trichoderma at soil water potentials approaching saturation. Experiments using onion seedling bioassays showed that the efficacy of Trichoderma isolates for the control of white rot using the same selection of soils and S. cepivorum isolates was variable, but that there was significant disease control overall. The importance of environmental factors and pathogen isolate in relation to effective biological control of white rot is discussed.
    Type of Medium: Electronic Resource
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