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Effects of infauna harvesting on tidal flats of a coastal lagoon (Ria Formosa, Portugal): Implications on phosphorus dynamics

机译:捕捞盗贼对沿海泻湖潮滩的影响(Ria Formosa,葡萄牙):对磷动力学的影响

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The systematic collection of benthic organisms in tidal flats of coastal lagoons should be taken into account for the management of these systems, once sediment disturbance affects biogeochemical processes by favouring pore water renewal during tidal inundation. The objective of the present work was to evaluate the effects of infauna harvesting on the phosphorus dynamics of muddy and sandy intertidal areas in the Ria Formosa. Sediment cores and overlying water were collected during August 2000 and February 2001 from reworked and undisturbed sediment before and after flooding. Results obtained showed that during the first minutes of flooding there was a marked decrease of phosphate in pore water of disturbed sediments. However, phosphate tidal fluxes from sandy sediment were clearly higher (17 nmol cm~(-2) d~(-1) in summer and 3 nmol cm~(-2)d~(-1) in winter) than in muddy sediment (0.4 nmol cm~(-2) d~(-1) in summer and —0.01 nmol cm~(-2) d~(-1) in winter). After muddy sediment disturbance concentrations of iron oxides increased quickly (from 5 to 16 μmol g~(-1)) and phosphate was sorbed onto these iron oxides, resulting in a buffering of phosphate pore water concentrations at low values in the oxidized sediment zone. The estimated P-output from muddy sediment decreased one to two orders of magnitude after sediment disturbance in contrast to sandy sediments in which the impact of infauna harvesting was minimal. Consequently, the P-cycle is influenced by the disruption of muddy habitats in tide-driven systems. Such information could be useful for the management of the lagoon.
机译:一旦沉积物扰动通过在潮汐淹没过程中促进孔隙水更新而影响了生物地球化学过程,就应考虑在沿海泻湖的滩涂中对底栖生物进行系统收集。本工作的目的是评估捕捞信息对福尔摩沙河(Ria Formosa)的泥泞和沙质潮间带磷素动力学的影响。在洪水之前和之后,于2000年8月和2001年2月从返工和未扰动的沉积物中收集了沉积物芯和上覆水。获得的结果表明,在洪水的前几分钟,受干扰的沉积物的孔隙水中磷酸盐的含量显着下降。然而,沙质沉积物中的磷酸盐潮通量明显高于泥质沉积物(夏季为17 nmol cm〜(-2)d〜(-1),冬季为3 nmol cm〜(-2)d〜(-1)。 (夏季为0.4 nmol cm〜(-2)d〜(-1),冬季为-0.01 nmol cm〜(-2)d〜(-1))。在泥泞的沉积物扰动之后,氧化铁的浓度迅速增加(从5到16μmolg〜(-1)),磷酸盐被吸附到这些氧化铁上,从而在氧化的沉积物区域中以较低的值缓冲了磷酸盐孔隙水的浓度。泥沙引起的泥沙流失后,估计的磷输出量减少了1-2个数量级,而沙质沉积物的捕捞活动影响最小。因此,P周期受潮汐驱动系统中泥泞生境的破坏影响。这样的信息对于泻湖的管理可能是有用的。

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