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Nitrification and inorganic nitrogen distribution in a large perturbed river/estuarine system: the Pearl River Estuary, China

机译:大型河床—河口系统的硝化作用和无机氮分布:珠江口,中国

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We investigated the spatial distribution and seasonal variation of dissolvedinorganic nitrogen in a large perturbed estuary, the Pearl River Estuary,based on three cruises conducted in winter (January 2005), summer (August 2005)and spring (March 2006). On-site incubation was also carried out fordetermining ammonium and nitrite oxidation rates (nitrification rates). Weobserved a year-round pattern of dramatic decrease in NH4+,increase in NO3−, but insignificant change in NO2− inthe upper estuary at salinity ~0–5. However, species andconcentrations of inorganic nitrogen at upper estuary significantly changed withseason. In winter, with low runoff, the most upper reach of the Pearl RiverEstuary showed relatively low rates of ammonia oxidation (0–5.4 μmolN L−1 d−1) and nitrite oxidation (0–5.2 μmol N L−1 d−1),accompanied by extremely high concentrations of ammonia (up to>800 μmol L−1) and nitrate (up to >300 μmol L−1). Insummer, the upper estuary showed higher nitrification rates (ammoniaoxidation rate ~1.5–33.1 μmol N L−1 d−1, nitriteoxidation rate ~0.6–32.0 μmol N L−1 d−1) with lowerconcentrations of ammonia (<350 μmol L−1) and nitrate (<120 μmol L−1).The Most Probable Number test showed relatively lowernitrifier abundance in summer at most sampling stations, indicating agreater specific nitrification rate per cell in the warm season. Temperatureappeared to control nitrification rates to a large degree in differentseasons. Spatial variability of nitrification rates appeared to becontrolled by a combination of many other factors such as nutrientconcentrations, nitrifier abundance and dissolved oxygen (DO)concentrations. In addition to aerobic respiration, nitrificationcontributed significantly to the consumption of DO and production offree CO2 at upper estuary. Nitrification-induced consumption accounted for up toapproximately one third of the total water column community DO consumptionin the upper estuary during the surveyed periods, boosting environmentalstress on this large estuarine ecosystem.
机译:我们基于冬季(2005年1月),夏季(2005年8月)和春季(2006年3月)进行的三次巡游,调查了一个大型扰动河口珠江口的溶解性无机氮的空间分布和季节变化。还进行了现场培养以确定铵和亚硝酸盐的氧化速率(硝化速率)。我们观察到全年NH 4 + 急剧下降,NO 3 -上升的模式,但微不足道盐度约为0-5时,上口NO 2 -的变化。然而,河口上部无机氮的种类和浓度随季节而显着变化。冬季,径流量低,珠江口上游最大,氨氧化率较低(0–5.4μmolNL -1 d -1 )氧化(0–5.2μmolNL -1 d -1 ),并伴随着极高浓度的氨(高达800μmolL -1 )和硝酸盐(高达> 300μmolL -1 )。夏季,河口上游的硝化率较高(氨氧化率〜1.5–33.1μmolNL -1 d -1 ,亚硝酸盐氧化率〜0.6–32.0μmolNL − 1 d −1 )氨(<350μmolL -1 )和硝酸盐(<120μmolL -1 )的浓度较低>)。最可能数试验显示,大多数采样站的夏季硝化剂丰度相对较低,表明在温暖季节每个细胞的比硝化率更高。在不同季节,似乎出现温度以在很大程度上控制硝化速率。硝化速率的空间变异性似乎是由许多其他因素共同控制的,例如营养物浓度,硝化剂丰度和溶解氧(DO)浓度。除有氧呼吸外,上口河口硝化还显着促进了DO的消耗和游离CO 2 的产生。在调查期间,硝化诱导的消耗量约占上河口水柱群落溶解氧消耗总量的三分之一,这加剧了这个大型河口生态系统的环境压力。

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