因无茶而冷淡 发表于 2025-3-28 18:16:18
Fronts and Mesoscale Features in the St. Lawrence Estuary,The influence of freshwater input, wind forcing and tidal processes on the distribution of temperature, salinity and current fields are discussed. Mechanisms responsible for variability of frontal phenomena, eddy formation and coastal jet dynamics are considered as a function of seasonal changes inN斯巴达人 发表于 2025-3-28 22:18:43
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Recent Sediments and Sediment Transport Processes in the St. Lawrence Estuary,y of the St. Lawrence Upper and Lower Estuaries. On the channel floor, ice contact facies overlain by post-glacial transgressive (Goldthwait) muds form two distinct stratigraphic units under gravel and sand lag deposits, and contemporaneous estuarine silty clays. The upper region is mostly shallow (OMIT 发表于 2025-3-29 04:50:50
Nearshore Sediment Dynamics in the St. Lawrence Estuary,400 km long, 70 km wide near the mouth and 15 km wide at the upper end. The dimensions of the Estuary are such that the hydrodynamic conditions prevailing in the lower portion are typically marine while those prevailing in the upper portion are typically estuarine. The tide is semi-diurnal and reachAUGUR 发表于 2025-3-29 07:24:14
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Sediment-Water Interaction and Early Diagenesis in the Laurentian Trough,review is made of the role of organic matter (input to the sediment surface, inmixing through bioturbation, degradation by bacteria) and of the distributions of oxidants, nutrients, trace metals and other chemical substances either directly and indirectly involved in the cycling of organic matter. MRENAL 发表于 2025-3-29 20:22:27
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