Monomictic Lake(單人湖)到底是什麼？
Monomictic Lake 單人湖 - A simple 1-D energy budget model (SIMO) for the prediction of the vertical temperature profiles in small, monomictic lakes forced by a reduced number of input meteorological variables is proposed. [1] , from exudation and lysis), meets phytoplankton P uptake and how it is associated with phytoplankton community composition changes under thermally stratified DIP-depauperate conditions in a large warm-monomictic lake. [2] Spatial and seasonal patterns reflected the bathymetry and previously described mixing patterns of this monomictic lake: warming of shallow bays in spring extended to wider area along with summer stratification period, while mixing of the water column was reflected in spatially more homogenous SWT in fall-winter. [3] The study investigated the metallothionein (MT) and glutathione peroxidase (GPX) genes expression in freshwater fish Cyprinus carpio dwelling in Warm-monomictic Lake (Dal) and Government culture pond. [4] Ecosystem dynamics in monomictic lakes are characterized by seasonal thermal mixing and stratification. [5]提出了一種簡單的一維能量收支模型 (SIMO)，用於預測由於輸入氣象變量數量減少而導致的小型單一湖泊中的垂直溫度剖面。 [1] ，來自滲出和溶解），滿足浮游植物對 P 的吸收，以及它如何與大型溫暖單組湖泊中熱分層 DIP 貧化條件下的浮游植物群落組成變化相關聯。 [2] 空間和季節模式反映了這個單一湖泊的水深測量和先前描述的混合模式：春季淺海灣的變暖隨著夏季分層期擴大到更廣泛的區域，而水柱的混合則反映在空間上更均勻的秋冬季 SWT . [3] 該研究調查了生活在暖單組湖 (Dal) 和政府養殖池中的淡水魚 Cyprinus carpio 中金屬硫蛋白 (MT) 和穀胱甘肽過氧化物酶 (GPX) 基因的表達。 [4] 單體湖泊的生態系統動力學以季節性熱混合和分層為特徵。 [5]
Warm Monomictic Lake 溫暖的莫諾蒂克湖
Vertical circulation reaches the bottom of the deepest (> 90 m) part of the northern basin of Lake Biwa, a warm monomictic lake, during winter (January to March) every year. [1] The lake is known to be a warm monomictic lake, thermally stratified through most of the year with the exception of winter, when small thermal vertical gradients permit mixing from top to bottom. [2] The present work describes the benthic macroinvertebrate communities of three tropical, warm monomictic lakes in “Lagunas de Montebello” National Park, Mexico, by describing the differences along the bathymetric profile, from the littoral down to the profound benthos. [3] 20 mg/L) using surface sediments of Lake Yangzonghai, a warm monomictic lake in southwestern China. [4] Vertical profiles of dissolved oxygen (DO) and water temperature (WT) measured bi-monthly for 36 years (1980–2015) near the deepest part of a warm monomictic lake were analyzed with special reference to yearly minimum DO at bottom (DOmin). [5]每年冬季（1 月至 3 月），垂直環流到達琵琶湖北部盆地最深處（> 90 米）底部，這是一個溫暖的單體湖。 [1] 眾所周知，該湖是一個溫暖的單體湖，一年中的大部分時間都是熱分層的，除了冬季，當小的熱垂直梯度允許從上到下混合時。 [2] 目前的工作描述了墨西哥“Lagunas de Montebello”國家公園三個熱帶、溫暖的單體湖泊的底棲大型無脊椎動物群落，通過描述沿水深剖面的差異，從沿海到深海底棲生物。 [3] 20 mg/L) 使用中國西南部溫暖的單體湖陽宗海湖的表層沉積物。 [4] 36 年來（1980-2015 年）每兩個月測量的溶解氧（DO）和水溫（WT）垂直剖面在溫暖的單體湖最深處進行了分析，特別參考了底部的年最低 DO（DOmin）。 [5]
Deep Monomictic Lake
In this study, carried out from the littoral (S1), pelagic (S2-S4), and the deepest site (S5), water samples from different depths and sediment cores were collected along the transect of Lake Fuxian, a deep monomictic lake to investigate the spatial–temporal variations of CH 4. [1] This study highlights the concern that in deep monomictic lakes, eutrophication restoration might be hindered by extensive internal P cycling and reduced capacity of sediment P-trapping. [2]在這項研究中，從沿岸 (S1)、遠洋 (S2-S4) 和最深處 (S5) 進行，沿深單組湖撫仙湖的橫斷面採集了不同深度和沈積物岩心的水樣，以研究 CH 4 的時空變化。 [1] 這項研究強調了在深層單體湖泊中，富營養化恢復可能會受到廣泛的內部磷循環和沈積物捕磷能力降低的阻礙。 [2]