半封闭浅海的岸线工程与水交换临界Shoreline engineering and exchange thresholds in a semi-enclosed shallow sea
环渤海的关键在于平均水深约 18 m 的半封闭浅海、水体交换时间长、四十多条入海河流和港口围填海共同改变潮流、泥沙、营养盐和污染物停留。夏季底层溶解氧下降、局地低氧、赤潮和湿地退化表明,岸线工程与陆源 C/N/P 输入已经耦合为同一条风险链 The Bohai Rim is a semi-enclosed shallow sea with an average depth of about 18 m, long water residence, more than forty inflowing rivers, and port-led reclamation that together change tidal currents, sediment, nutrients, and pollutant retention. Summer bottom-oxygen decline, local hypoxia, HABs, and wetland degradation place shoreline engineering and land-based C/N/P inputs in the same risk chain.
- 围填海形态、潮汐交换时间和陆源 C/N/P 滞留共同约束半封闭浅海的物质停留Reclamation geometry, tidal exchange time, and land-based C/N/P retention constrain material residence in a semi-enclosed shallow sea.
- 湿地退化、赤潮、缺氧和生物多样性下降呈现连续的生态风险信号Wetland degradation, HABs, hypoxia, and biodiversity loss form a continuous sequence of ecological risk signals.
环渤海临界诊断集中在人工岸线比例、潮汐交换时间、底层溶解氧、营养盐滞留、潮滩湿地面积和赤潮频次Bohai diagnosis centers on artificial shoreline share, tidal exchange time, bottom dissolved oxygen, nutrient retention, tidal-flat wetland area, and HAB frequency.