机译:切萨皮克湾中海湾沉积物中的有机质再矿化作用主要是磷循环。
Department of Plant and Soil Sciences, University of Delaware, Newark, Delaware 19716, United States;
EnvironmentaI Molecular Science Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99354, United States;
Department of Ocean, Earth, and Atmospheric Sciences, Old Dominion University, Norfolk, Virginia 23529, United States;
EnvironmentaI Molecular Science Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99354, United States;
Department of Plant and Soil Sciences, University of Delaware, Newark, Delaware 19716, United States;
Department of Plant and Soil Sciences, University of Delaware, Newark, Delaware 19716, United States;
机译:大陆边缘沉积物中的碳循环:有机质特征与再矿化率和途径之间的对比
机译:切萨皮克湾沉积物孔隙水中溶解的有机物
机译:中盐在切萨皮克湾沉积物中的碳循环2:颗粒动力学和溶解的有机碳周转
机译:Duliujianhe河表面沉积物总氮,总磷和有机物的空间分布特征
机译:夏威夷凯内奥赫湾及其周围沿海沉积物中的有机物再矿化
机译:营养不足的湿地沉积物易受微生物群变化和汞循环的影响并添加了溶解有机物
机译:密西西比湾沉积物磷循环:有机磷的作用和季节性氧化还原涨落
机译:切萨皮克湾干流中湾和侧站水质数据的比较:切萨皮克湾计划