hypolimnetic

基本解釋

Hypolimnion The lower noncirculating water in a thermally stratified lake.
下層滯水層，均溫層：在熱層結(jié)湖中位置較低的不循環(huán)水層。
Hypolimnetic oxygen diffusers increase sediment oxygen demand (SOD) and, if not accounted for in design, can further exacerbate anoxic conditions.
溶氧量在環(huán)境與生物體皆扮演一個(gè)重要的角色，包括生物體生化醫(yī)藥、食品工業(yè)、廢水處理以及水產(chǎn)養(yǎng)殖等。
In many lakes in summer that is a warm low-density layer (EPILIMNION) lying above a colder denser layer (the HYPOLIMNION), the zone of rapid temperature change between the two layers being celled the thermocline.
夏季，多數(shù)湖中溫暖的低密度水層（湖面溫水層）在寒冷的較高密度水層（湖底凈水層）之上，中間夾有溫度改變較快的水層（變溫層）。
metalimnion A zone of abrupt temperature change (thermocline) between the warm epilimnion and the cool hypolimnion of a lake.
變湖層在湖的溫暖表水層與冷的深水層之間的一個(gè)突然溫度改變(斜溫層)的區(qū)域。
hypolimnion The cold lower layer of a straitfield lake, under the epilimmion and beginning just below the thermocline. This layer is not directly affected by surface events.
斜溫層下水分層湖的寒冷低層，在斜溫層上水下方與斜溫層正下方開(kāi)始。這一層并不直接被表面事件影響。