自然の流れと水力工場の遺産
Robert C Walter1, Dorothy J Merritts
1Department of Earth and Environment, Franklin and Marshall College, Post Office Box 3003, Lancaster, PA 17604-3003, USA. robert.walter@fandm.edu
まとめ
中大西洋の小川は,歴史的に,湿地の枝分かれする運河であり,曲がりくねった川ではありませんでした. ミルダムにより沈殿物が蓄積され,人工の平原が形成され,川の回復モデルに挑戦されました.
科学分野:
- ジオモルフォロジー ジオモルフォロジー
- 環境の歴史 環境史
- 修復エコロジー 修復エコロジー
背景:
- 砂利床の小川は,細粒子の洪水平原を持つ曲がりくねった川として広くモデル化されています.
- このモデルは,流れの回復の取り組みに大きな影響を与えます.
研究 の 目的:
- 中大西洋流の歴史的地形を再評価する.
- 現代の流域の形成を調査し,既存の流域モデルに異議を唱える.
主な方法:
- 流の堆積物の地質的地図作成と年代測定.
- 歴史的地図と記録の分析. 歴史的地図と記録の分析.
主要な成果:
- 定住前の川は,湿地の内部に枝分かれする運河であり,有機炭素を貯蔵していました.
- 17世紀から19世紀のミールダムの後ろにある1〜5メートルの堆積堆積は,これらの湿地を埋葬しました.
- 大西洋中部の洪水平原のほとんどは,人工的な充填テラスとして識別されています.
結論:
- 曲がりくねった小川と洪水平原の広く受け入れられているモデルは,人為的に変化した風景に基づいています.
- 歴史的に切断された運河は,曲がりくねった川の復元のための自然な原型ではありません.
- 復元慣行は,入植前の湿地の条件に基づいて再評価する必要があるかもしれません.
関連する概念動画
Freshwater Microbial Ecology
Freshwater systems such as streams, rivers, and lakes exhibit distinct physical and biological characteristics that influence their microbial communities. These environments are broadly categorized into lotic systems—those with flowing waters like streams and most rivers—and lentic systems, which include still or slow-moving waters such as lakes, ponds, and marshes.In lentic systems, phytoplankton drive primary production, generating autochthonous organic carbon. In contrast, lotic systems...
Laminar Flow
Laminar flow represents a smooth, orderly fluid motion where particles move along parallel paths, resulting in minimal mixing between layers. Streamlined particle paths characterize this flow regime and occur under conditions where viscous forces dominate over inertial forces. The distinction between laminar, transitional, and turbulent flow is primarily determined by the Reynolds number, a dimensionless quantity calculated as:
Gradually Varying Flow
Gradually varying flow (GVF) in open channels describes situations where water depth changes slowly along the channel due to factors like non-uniform bed slope, channel shape variations, or obstructions. This flow type occurs when the depth adjusts gradually to balance gravitational forces, shear forces, and energy requirements, resulting in a low rate of depth change.Characteristics of Gradually Varying FlowGVF is commonly observed in natural streams, rivers, and canals, where flow depth...
Streamlines, Streaklines, and Pathlines
A streamline represents the trajectory that is always tangent to the fluid's velocity vector at any given point. The velocity of a fluid particle is always directed along the streamline, ensuring the particle continuously follows the streamline's path. Streamlines are particularly useful for visualizing the overall direction of flow in a fluid system, and they provide an instantaneous representation of the flow's velocity field. In steady flow, where conditions do not change over time,...
Underflow Gates
Underflow gates are vital for controlling water flow in irrigation canals. The three main types of underflow gates — vertical, radial, and drum gates — serve different purposes while ensuring effective flow management. Vertical gates move up and down, generating a free-flowing water jet; radial gates pivot to regulate the flow; and drum gates rotate for precise adjustments. The flow through these gates is influenced by downstream conditions, resulting in free or drowned outflow.Free and Drowned...
Weir
A weir is a hydraulic structure designed to partially obstruct an open channel, enabling precise control and measurement of water flow. By forcing water to flow over or through it, a weir allows for accurate determination of discharge rates, making it an essential tool in water resource management. These structures are extensively used in regulating river flows, irrigation systems, and flood control channels.Types of Weirs and Their FeaturesWeirs are categorized primarily into sharp-crested and...


