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Spatial and temporal changes of phosphorus in coastal wetland soils as affected by a tidal creek in the Yellow River Estuary, China

机译:黄河口潮汐对沿海湿地土壤磷的时空变化影响

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In order to investigate spatial and temporal changes of soil phosphorus and its availability in coastal wetlands in the Yellow River Estuary, soil samples from five sampling sites (Sites 1-5) in four sampling periods were collected and the contents of soil phosphorus and other properties were detected. Our results showed that there were no significant differences in total phosphorus (TP) in surface and subsurface soils among the five sampling sites (p > 0.05), whereas significant differences were observed between June and other months (p < 0.05) following the order June > August > November > April. Generally, available phosphorus (AP) contents also showed a fluctuation in different sampling periods and there were significant differences between November and August and April at 10-20 cm soil layer (p < 0.05). The soil P supply was generally lower with lower AP:TP ratios less than 2%. Spatial changes along the sampling belt in AP: TP ratios were similar in surface soils except for April, whereas they decreased in subsurface soils in June and November, and fluctuated slightly in August and April. Lower C:P ratios (<50) in coastal wetland soils contributed to soil P mineralization. Spatial changes in the C:P ratios were similar the surface soils in four sampling periods, and the reverse changing tendencies were observed in subsurface soils between April and June and between August and November. Correlation analysis showed that TP had significant positive correlations with Al, Mg and bulk density and negative correlations with soil moisture and C:P ratio (p < 0.01). Comparatively, AP was just significantly correlated with soil organic matter. The findings indicated that seasonal changes in soil P should be given more concerns to minimize the eutrophication risk of water bodies in coastal wetlands and guide the flow and sediment regulation regime of the upstream reservoir. (C) 2015 Elsevier Ltd. All rights reserved.
机译:为了调查黄河口沿海湿地土壤磷的时空变化及其有效性,收集了四个采样期内五个采样点(1-5处)的土壤样品,并分析了土壤磷含量及其他性质被检测到。我们的结果表明,在五个采样点之间,表层和地下土壤中的总磷(TP)均无显着差异(p> 0.05),而在6月份之后的6月与其他月份之间则观察到显着差异(p <0.05)。 >八月>十一月>四月。通常,有效磷(AP)含量在不同的采样时期也显示出波动,在11-20年的土壤层(10-20厘米)之间有显着差异(p <0.05)。土壤磷的供应通常较低,而较低的AP:TP比值不到2%。除4月外,表层土壤中沿AP:TP比的空间变化相似,而6月和11月在地下土壤中则有所下降,而8月和4月则略有波动。沿海湿地土壤中较低的C:P比(<50)导致土壤P矿化。 C:P比的空间变化在四个采样周期内与表层土壤相似,并且在4月至6月之间以及8月至11月之间在地下土壤中观察到了相反的变化趋势。相关分析表明,TP与Al,Mg和堆积密度呈显着正相关,与土壤水分和C:P比呈负相关(p <0.01)。相比之下,AP与土壤有机质之间的相关性显着。研究结果表明,应更加关注土壤P的季节性变化,以最大程度降低沿海湿地水体富营养化的风险,并指导上游水库的水流和泥沙调节方案。 (C)2015 Elsevier Ltd.保留所有权利。

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