热带河口潜在的富营养化与虾污水中磷的输入

Rafael Aquino, S. Rodrigues, P. Souza-Filho, Silvia K. Kawakami
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引用次数: 0

摘要

由于产生富含有机物和营养物的废水,虾养殖与富营养化有关。利用表层沉积物和沉积物岩心研究了巴西东北部Coreaú河口沉积物中磷的分布。在表层沉积物中,总磷浓度为349.2 ~ 633.5 μg -1(平均值为465.2),比巴西其他受大型对虾养殖影响的河口低约3倍。表层沉积物中磷的优势形态依次为:铁结合磷(Fe-P, 30%) >有机磷(orgp, 23%) >交换磷(Exch-P, 20%) >自生磷灰石(Ca-P, 15%) >碎屑磷灰石(De-P, 12%)。Exch-P与Fe-P无显著相关(r = 0.389;P < 0.05)。Exch-P和Org-P浓度最高,且两者之间存在较强的相关性(r = 0.706, p < 0.05),说明土壤中磷和有机质来源相同。河口(T1)和河口上游(T2)沿岩心的总磷积累量分别为10211和15632 μg -1。T1的优势序列为De-P (36%) > Ca-P (25%) > Fe-P (22%) > Exch-P (9%) > Org-P (7%);而T2表明:磷(31%)> De-P (23%) > Org-P (21%) > Ca-P (17%) > Exch-P(9%)。磷素沉积史指向20世纪80年代末和90年代中期的磷素积累期,与城市化进程加快和养虾场开始或最活跃的时期相一致。尽管总磷浓度较低,但表层沉积物中活性形态Exch-P、Fe-P和Org-P的比例显示出高富营养化潜力的趋势。
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Potential Eutrophication Associated with Phosphorus Inputs from Shrimp Effluents in a Tropical Estuary
Shrimp farming has been associated with eutrophication due to the generation of effluents enriched with organic matter and nutrients. Phosphorus (P) distribution was investigated in the Coreaú River Estuary (NE Brazil) using surface sediments and sediment cores. In surface sediments, total P concentrations ranged from 349.2 to 633.5 μg g-1 (mean = 465.2) and were about three times lower than those of other Brazilian estuaries impacted by larger shrimp cultures. The predominance of P forms in surface sediments followed the sequence: iron-bound P (Fe-P, 30%) > organic-P (Org-P, 23%) > exchangeable-P (Exch-P, 20%) > authigenic apatite (Ca-P, 15%) > detrital apatite (De-P, 12%). No significant correlation was observed between Exch-P and Fe-P (r = 0.389; p < 0.05). Highest Exch-P and Org-P concentrations and a strong correlation between these forms were found (r = 0.706, p < 0.05), suggesting the same sources of P and organic matter. Total P accumulation along the cores was 10,211 and 15,632 μg g-1 at the estuary mouth (T1) and the upper estuary (T2), respectively. T1 exhibited the predominant sequence: De-P (36%) > Ca-P (25%) > Fe-P (22%) > Exch-P (9%) > Org-P (7%); whereas T2 showed: Fe-P (31%) > De-P (23%) > Org-P (21%) > Ca-P (17%) > Exch-P (9%). Phosphorus depositional history points to P accumulation episodes at the end of the 1980 and mid-1990, coinciding with increasing urbanization and the beginning or maximum activity of the shrimp farms. Despite the low total P concentrations, the proportions of the labile forms Exch-P, Fe-P and Org-P in surface sediments indicated a trend to a high potential for eutrophication.
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