三种鱼的磷排泄及其在微型生态系统磷再循环中的作用

在考查罗非鱼或鲢、鳙下行影响的微型生态系统实验后期 ,对三种鱼的特定正磷酸盐 (PO4 P)排泄率进行了测定 ,并且估算了系统中实验鱼的PO4 P排泄率。结果表明 ,在个体大小相同的情况下 ,罗非鱼的特定PO4 P排泄率明显地高于链、鳙 ,似乎同它们的食物含磷量无关而由其体组织含磷量所决定 ;放养罗非鱼的系统中鱼的PO4 P排泄率比放养链、鳙的系统平均高 2倍多 ,其磷排泄对浮游植物的PO4 P供给率分别为 10 0 %— 15 8%和 6 1%—7 5 %。根据有鱼系统中PO4 P的供求关系和实验结束时磷分布的观测结果推断 ,沉积物的磷释放是系统中磷再生的主要途径 ,而实验鱼调节系统磷再循环的主要机制是排粪。     

PHOSPHORUS DYNAMICS IN THE MONIMOLIMNION OF SWARTVLEI

SUMMARY

The exchange of phosphorus between the bottom sediment and monimolimnion of Swartvlei, a meromictic, humic lake, was investigated during the last three months of 1980. The concentrations of oxygen, dissolved salts, phosphorus and Fe⁺⁺ in the water column were monitored, and electrode potentials in the bottom mud were measured, at approximately weekly intervals. At the same time laboratory experiments were performed, using Jenkin core samples, to observe the effect of changing oxygen concentration and salinity on phosphate exchange between sediment and water, and on electrode potentials at the sediment-water interface. Phosphorus was released under unaerobic conditions at a rate of 2,5 mg P m^?2 d^?1 and was taken up again under aerobic conditions at 1,6 mg P m^?2 d^?1 These values were in agreement with existing observed data on changes in phosphate concentration.     

CHARACTERISTICS OF PHOSPHORUS DEFICIENCY IN ANABAENA1

Several aspects of the metabolism and composition of a strain of Anabaena have been studied during phosphorus deficiency. The effects of medium composition, substrate concentration, temperature, pH, and illumination on alkaline phosphatase activity and phosphate uptake have been examined. Of particular interest among these results was the dependence of maximum alkaline phosphatase activity on Ca and of phosphate uptake on Mg. Depletion of dissolved phosphate from the culture medium runs accompanied by a marked increase in alkaline phosphatase activity, initial rate of phosphate uptake, and total amount of phosphate taken up to satisfaction of the phosphorus debt. Readdition of phosphate to a phosphorus-deficient culture resulted in a rapid decline in the ability to take up phosphate but no loss of alkaline phosphatase beyond dilution of activity already present. Entry into phophorus deficiency was accompanied by a loss of heterocysts, a decline in chlorophyll a, protein, RNA, and cellular phosphorus, and an increase in carbohydrate per unit dry weight. The possible use of these changes as physiological indicators of phosphorus limitation in natural situations is discussed.     

不同水平磷对磷饥饿墨兰某些生化特性的影响

本文研究不同水平磷对磷饥饿墨兰［Ｃｙｍｂｉｄｉｕｍｓｉｎｅｎｓｅ（Ａｎｄｒ．）Ｗｉｌｌｄ］植株某些生化特性的影响．随着ＮａＨ２ＰＯ４浓度的增高,植株中的无机磷酸、磷脂酸、肌醇六磷酸、磷酸已糖、高能磷酸化合物和核酸等的含量都有不同程度的提高,其中以肌醇六磷酸提高最显著．酸性磷酸酯酶活性与磷浓度呈负相关．０．２０ｍｍｏｌ／ＬＮａＨ２ＰＯ４可能基本满足墨兰植株生长的要求．缺磷时叶片的蛋白质、无机磷酸和可溶性糖的含量较低,而游离氨基酸和淀粉的含量较高．因此,缺磷条件下生长的植株矮小的原因,可能主要是缺乏蛋白质。     

磷在羊草草地植物－土壤中积累、分布及转移规律

本文在研究磷素几种形态的动态变化基础上,运用生态系统理论,利用系统分析的方法,分析了磷在植物－土壤系统中的流通、积累和归还的特点,得出如下结果：１．磷素在系统内９９％以上分布在土壤中。２．群落内磷的再利用量为３．６７５５ｋｇ·ｈａ￣（－１）·ｙｒ￣（－１）。３．群落每年吸收的磷为３．４０６３ｋｇ·ｈａ￣（－１）·ｙｒ￣（－１）,地上部归还土壤为０．１４４７ｋｇ·ｈａ￣（－１）·ｙｒ￣（－１）,地下部归还土壤为１．８１１１ｋｇ·ｈａ￣（－１）·ｙｒ￣（－１）,输出仅占吸收量的４２．２４％,磷素在群落中每年净积累为０．３５ｋｓ·ｈａ￣（－１）·ｙｒ￣（－１）。４．磷在各库内的周转时间是：地上植物活体为１．３３６４年,立枯体为６．４３５０年,活根为１．０８８７年,死根为２．４３７８年,有机磷为８３３．３年。     

不同固磷方式对巢湖沉积物磷吸附行为的影响

内源磷负荷将严重阻碍富营养化湖泊的恢复,其控制技术的关键在于有效增强沉积物吸附磷的能力,而相关研究相对较少。研究以典型富营养化湖泊(巢湖)严重污染区域的沉积物为实验对象,系统比较了常规固磷方式(施用CaCl2、FeCl3、AlCl3与曝气)对沉积物磷吸附行为和间隙水溶解态可反应磷(SRP)浓度的影响。结果表明:施用不同剂量的CaCl2之后,沉积物磷最大吸附量和吸附能均无显著变化,间隙水SRP浓度和沉积物磷平衡浓度(EPC0)仅有较小幅度的下降;FeCl3和AlCl3的施用可明显增加沉积物磷的最大吸附量和吸附能,同时有效降低间隙水SRP浓度和EPC0值,即沉积物显示更强的从水中吸附磷的能力。当同处低剂量水平时,铁能更有效地降低沉积物EPC0值;反之,曝气对沉积物最大吸附量和吸附能均无显著影响,却明显提高了间隙水SRP浓度和沉积物EPC0值,进而导致更强的磷释放风险。故建议将适量铁的施用作为富营养化湖泊沉积物修复的有效技术,且慎用曝气处理。     

THE ROLE OF PERIPHYTON IN PHOSPHORUS RETENTION IN SHALLOW FRESHWATER AQUATIC SYSTEMS

Eutrophication caused by phosphorus (P) leads to water quality problems in aquatic systems, particularly freshwaters, worldwide. Processing of nutrients in shallow habitats removes P from water naturally and periphyton influences P removal from the water column in flowing waters and wetlands. Periphyton plays several roles in removing P from the water column, including P uptake and deposition, filtering particulate P from the water, and attenuating flow, which decreases advective transport of particulate and dissolved P from sediments. Furthermore, periphyton photosynthesis locally increases pH by up to 1 unit, which can lead to increased precipitation of calcium phosphate, concurrent deposition of carbonate-phosphate complexes, and long-term burial of P. Actively photosynthesizing periphyton can cause super-saturated O₂ concentrations near the sediment surface encouraging deposition of metal phosphates. However, anoxia associated with periphyton respiration at night may offset this effect. Linking the small-scale functional role of periphyton to ecosystem-level P retention will require more detailed studies in a variety of ecosystems or large mesocosms. A case study from the Everglades illustrates the importance of considering the role of periphyton in P removal from wetlands. In general, periphyton tends to increase P retention and deposition. In pilot-scale constructed periphyton-dominated wetlands in South Florida, about half of the inflowing total P was removed.     

陆地生态系统磷素循环及其影响因素

 磷是生命系统的重要组成成分,其在生态系统内的迁移转化是生态系统结构和功能的决定性因素之一。近20年来,磷在陆地生态系统内的重要性受到越来越多的关注。该文总结了国内外磷循环研究的成果,从磷的来源、在土壤中的存在形态和固定特性、影响因素的复杂性等方面分析了磷素循环的特点;系统阐述了磷在陆地生态系统各库之间及其内部,主要是植被-土壤亚系统内的迁移转化规律及影响因素。陆地生态系统磷素循环主要是系统内部的生物化学循环,由植物自身的遗传特性和土壤的生物、理化性质共同控制,不同控制因素的相对重要性因生态系统类型、时间和空间尺度而异。文章简述了磷循环研究方法的发展及存在的局限性;另外,分析了干旱、半干旱地区磷循环研究的重要性和意义;干旱区生态系统的脆弱性及其植被、土壤特性决定了其磷素循环有其自身的特点及研究的必要性。最后指出了当前陆地生态系统磷循环研究的发展趋势。     

富营养化湖泊沉积物磷原位控制技术

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底栖藻类对消落带土壤中各形态磷的影响

为揭示底栖藻类对三峡库区消落带淹没初期土壤中不同形态磷的影响作用,开展了相关的模拟实验。结果表明,在模拟的底栖藻类影响条件下,消落带土壤中铝磷（Al-P）的含量在实验期间处于波动状态,Al-P相对于其余形态的磷更易于被藻类吸收利用,且与藻类生长存在密切相关,即底栖藻类生长状态较好时,土壤中Al-P呈现下降趋势;而生长状态较差时,土壤中Al-P又出现略微上升的趋势。在实验后期土壤中Al-P含量上升,可能是其余形态的磷转化而来。底栖藻类的生长对不同深度土壤中铁磷（Fe-P）的影响不同,其生长对2-4 cm层土壤的影响较大,而对其余层影响不大。不同深度土壤中闭蓄态磷（O-P）和钙磷（Ca-P）含量差异不明显。实验后期Fe-P、O-P和Ca-P含量一直呈现下降的趋势,只有Al-P在后期出现上升的趋势,说明在淹水条件和底栖藻类生物膜共同作用下,土壤磷的有效性提高,土壤中难溶性磷向易溶性磷转化。       

SIZE-DEPENDENT PHOSPHORUS UPTAKE KINETICS AND CELL QUOTA IN PHYTOPLANKTON1

The allometric equation, y = aX^b, described the interspecific variation of phosphate uptake kinetics and cell quota with phytoplankton cell size and showed that smaller cells are superior in uptake rate to large. Species-specific measurements, made by track autoradiography in phosphorus deficient cultures of communities from a phosphorus-limited lake, revealed that eight different species did not differ significantly in the Michaelis-Menten half-saturation constant, K_m. However, both saturated uptake rates (V_max) and the initial slope of the uptake curve (V_max:K_m) decreased per unit biomass with increasing cell size. Biomass-specific cell phosphorus quotas also decreased with increasing cell volume, but less rapidly than did V_max or V_max: K_m. Comparable data from the literature showed that marine species were superior in phosphorus uptake to freshwater species of similar size, but allometric variation of kinetics appeared to exist within both groups. Together with a variable internal stores model of phosphorus-limited growth, the allometric relationships of uptake kinetics and quotas predicted competition to favor smaller cells, with a differential in growth rate diminishing as competitive intensity increased.