Assessment of labile phosphorus fractions and adsorption characteristics in relation to soil properties of West African savanna soils

A large proportion of total P in the soils of the area is unavailable to plants and consequently P is the second most limiting nutrient. The labile and moderately labile phosphorus fractions and adsorption characteristics of surface and subsurface horizons of eleven soil profiles in the derived savanna (DS) and the northern Guinea savanna (NGS) of West Africa were assessed. The labile P fractions are the resin and HCO₃-extractable inorganic (Pi) and organic (Po) P. The moderately labile fractions are the NaOH-extractable portion of soil P in the Hedley sequential procedure. In the DS soils, the resin P, considered the most readily available fraction, varied from 1 to 14 mg kg⁻¹, HCO₃-Pi ranged from 3.3 to 11, and HCO₃-PO was between 4 and 12 mg kg⁻¹ in the surface horizon. In the NGS, the topsoil contained 1.5–3 mg kg⁻¹ of resin P, 5–8 mg kg⁻¹ of HCO₃-Pi, and 7.5–9.7 mg kg⁻¹ of HCO₃-Po. Sodium hydroxide-Po was the largest of the fractions in all the soils studied. It ranged from 23 to 55 mg kg⁻¹ in the topsoil. In general, the labile P levels were higher in soils of the DS than of the NGS and were related to the oxalate-extractable Fe (Fe_ox), and Al (Al_ox) as well as to soil texture. The subsoil of Kasuwan Magani (profile KS 9–21 cm) required 153 mg P kg⁻¹ to maintain 0.2 mg P l⁻¹ in solution (standard P requirement), and Danayamaka (profile DD 7–32 cm) required 145 mg P kg⁻¹. These could translate to 214 and 200 kg P ha⁻¹ if a plow layer of 10 cm is assumed. Because these are within the plow layer, more P fertilizer would be needed for crop production than in the other soils. The standard P requirement and the adsorption maxima were related to Fe_ox and Al_ox, dithionite-Fe (Fe_d), and texture. The increase in labile P content with decreasing Fe_ox and Al_ox could imply that management practices capable of reducing the activities of Fe and Al in solution might improve P availability.     

珠江广州市区河段磷的迁移和分布的初步研究

研究了珠江广州市区河段黄沙－员村全程１３１００ｍ水域和底泥中不同形态磷的含量分布。并探讨磷在水体和底泥中的转移途径，为水污染的防治提供科学依据。     

水培蔬菜法对富营养化水体中氮磷的去除特性研究

利用水培蔬菜法净化富营养化河水，考察了不同形态的氮磷在处理前后的变化，在此基础上阐明水培法去除富营养化水体中氮磷的过程与机理。     

沉积物中磷负荷及其释放对水质的影响

以华东师范大学校河为研究对象，通过野调研与室内模拟实验相结合，研究了校河沉积物中磷负荷量，释放量与释放速度以及温度和水体扰动对其影响，并探讨了沉积物中磷释放对校河水质的影响，为校河的富营养化防治提供科学依据。     

缺氧反硝化去除难降解杂环化合物吡啶研究

在实验室中，采用好氧、厌氧和缺氧间歇试验，研究焦化废水中一种难降解有机物--吡啶的生物降解性能。试验主要研究了在缺氧状态下吡啶的生物降解性能、适宜的N/C比、N源的变化情况等。研究结果表明，缺氧反硝化状态下吡啶的生物降解性能有显著的提高。     

流动注射荧光猝灭法测定环境水样中痕量磷

在硫酸溶液中，P(Ⅴ)与钼酸盐、钒酸盐生成磷钼钒杂多酸，使罗丹明6G荧光猝灭，据此建立了测定痕量磷的流动注射荧光猝灭方法。方法的测定范围为2～90μg／L,进样频率为35样/h。采用本法测定环境水样中痕量磷，结果令人满意。     

污水生物除磷研究进展

水体富营养化是世界性难题,其中磷通常是主要限制因子.生物除磷工艺简单,污泥产量少,可节约能源,运行费用也较低,便于操作和磷的回收.在介绍水体中磷的来源、污染特点及其造成危害的基础上,着重综述了国内外生物除磷的研究进展,并对生物除磷存在的问题和发展趋势提出了一些看法.     

硝酸盐浓度及投加方式对反硝化除磷的影响

采用SBR反应器，详细研究了硝酸盐浓度及其投加方式对反硝化除磷过程的影响。结果表明，缺氧环境下的反硝化吸磷速率与作为电子受体的硝酸盐浓度有很大的关系，硝酸盐浓度越高．吸磷速率越快。当硝酸盐浓度较低．不足以氧化反硝化聚磷菌细胞内的PHB从而导致体系反硝化除磷效率的下降。相同浓度的硝酸盐，采用流加的方式可以获得比一次性投加更高的反硝化吸磷速率。缺氧环境下，反硝化脱氮量与磷的吸收量成良好的线性关系．借助于反硝化聚磷菌，反硝化脱氮与除磷可在一种环境中完成，有效解决了废水中COD不足的问题．同时达到了节省能源和降低污泥产量的目的。     

Environmental impact of two successive chemical treatments in a small shallow eutrophied lake: Part I. Case of aluminium sulphate

This paper deals with the efficiency and effects of addition of aluminium sulphate on soft water quality of a shallow eutrophic lake. Almost all the controlled variables improved with treatment, especially nutrient concentrations such as soluble reactive phosphorus (SRP) and transparency. However, aluminium sulphate was not added in sufficient quantity to reduce the total phosphorus content. SRP concentration was significantly reduced in the short term. Moreover, external loading of phosphorus was high and not taken into account by the in-lake treatments. Finally, resuspension of sediment (polymictic lake) removed the alum hydroxide layer on the sediment surface, which reduced treatment effectiveness. No significant pH decrease was noted following alum addition. According to bibliographical toxicological data, monomeric aluminium content does not show any toxic effect on aquatic fauna and flora. In spite of low SRP in the water column, the treatment did not prevent appearance of Microcystis sp. colony (> 10 colony per ml) approximately 30 days after alum application.     

Effect of pH on Pb biouptake by the freshwater alga<Emphasis Type="Italic"> Chlorella kesslerii</Emphasis>

The effect of pH on Pb bioaccumulation by Chlorella kesslerii was studied. Both Pb uptake fluxes and Pb bound to membrane transport sites increased with an increase in pH from 4.0–5.0, were relatively stable in the pH interval 5.0–6.5, and increased again at pH 7.0 and 8.0. Protons affected Pb adsorption to the algal surface by competing directly for surface sites, by modifying the overall algal surface charge and by modifying the chemical speciation of Pb in solution. These results indicate a failure of the free-ion activity or biotic ligand models above pH 6.5, possibly due to the bioaccumulation of hydroxo or carbonato Pb complexes.