北亚热带3种典型森林群落对降水中氮、磷、硫的截留及分配特征

森林群落在净化空气、截留沉降污染物、改善地表水质等方面具有重要作用。本研究以北亚热带地区3种典型森林群落（毛竹林、杉木林、青冈阔叶林）为研究对象,通过分析沉降污染物（NH₄⁺-N、NO₃^--N、NO₂^--N、TP和SO₄^2-）在大气降水、林内穿透雨、树干茎流、枯透水和地表径流中的浓度和通量变化特征,探讨不同森林群落对氮、磷、硫的截留净化作用和分配特征。结果表明,该区域大气降水中NH₄⁺-N、NO₃^--N、NO₂^--N、TP和SO₄^2-年均浓度分别为1.06、0.61、0.04、0.07、1.84 mg/L,其年均pH为5.88;各森林群落林冠层能够调升降雨的pH且全年稳定,对TP和NH₄⁺-N均有吸附作用,截留率分别为79.09%-84.68%和30.88%-69.36%;而枯落物层则是林下氮、磷、硫的主要释放源,对NH₄⁺-N、NO₃^--N、TP和SO₄^2-均具有淋溶作用;此外,由地表径流（输出）与大气降水（输入）的对比分析可知,各林地对沉降污染物中氮、磷、硫的截留率均超过98%;3种森林群落对沉降污染物中氮、磷、硫的截留能力依次为：青冈阔叶林 > 毛竹林 > 杉木林,阔叶林对沉降污染物的净化能力要高于毛竹林及针叶的杉木林。     

Atmospheric deposition, mass balances, and processes regulating streamwater solute concentrations in mixed-conifer catchments of the Sierra Nevada, California

Solute concentrations in atmospheric deposition and stream water were measuredfrom 1984 through 1993 to determine the fate and mobility of solutes in twogauged mixed-conifer catchments (Tharp's and Log creeks) located in theSierra Nevada, California. The two catchments contain mature forest standsdominated by Abies concolor (white fir), Sequoiadendron giganteum (giantsequoia), Abies magnifica (red fir) and Pinus lambertiana (sugar pine).Ammonium, Cl^-, Ca²⁺ and NO^- ₃were highest in concentration of the solutes measured in wet deposition;bulk deposition was highest in SO^{2- 4}, NH⁺ ₄,Cl^- and H⁺. Net retention ofH⁺, NO₃ ^-, NH₄ ⁺,SO₄ ^2- and Cl^- occurred in both catchments.Discharge was dominated by spring snowmelt with the largest export yieldsfor acid neutralizing capacity (ANC), SiO₂, andCa²⁺. Export yields of H⁺,NO₃ ^-, NH₄ ⁺ and PO₄ ^3-were relatively small (0.5 kg ha^-1 y^-1).Discharge-concentration relationships for ANC, SiO₂,Na⁺, K⁺, Ca²⁺ andMg²⁺ were inverse and their concentrations in stream waterwere primarily influenced by discharge and annual differences in the relativecontributions of snowmelt and groundwater. The mobility of these solutes iscontrolled by the rates of mineral weathering and ion exchange. The positiverelationship of SO₄ ^2- concentration with increasingdischarge suggests that atmospherically deposited SO₄ ^2-is temporarily stored and that its release is controlled by the extent of soilwater flushing.     

Growth,chemical composition,and nitrate reductase activity of Rumex species in relation to form and level of N supply

Growth, chemical composition, and nitrate reductase activity (NRA) of hydroponically cultured Rumex crispus, R. palustris, R. acetosa, and R. maritimus were studied in relation to form (NH₄ ⁺, NO₃ ^-, or both) and level of N supply (4 mM N, and zero-N following a period of 4mM N). A distinct preference for either NH₄ ⁺ or NO₃ ^- could not be established. All species were characterized by a very efficient uptake and utilization of N, irrespective of N source, as evident from high concentrations of organic N in the tissues and concurrent excessive accumulations of free NO₃ ^- and free NH₄ ⁺. Especially the accumulation of free NH₄ ⁺ was unusually large. Generally, relative growth rate (RGR) was highest with a combination of NH₄ ⁺ and NO₃ ^-. Compared to mixed N supply, RGR of NO₃ ^-- and NH₄ ⁺-grown plants declined on average 3% and 9%, respectively. Lowest RGR with NH₄ ⁺ supply probably resulted from direct or indirect toxicity effects associated with high NH₄ ⁺ and/or low Ca²⁺ contents of tissues. NRA in NO₃ ^- and NH₄NO₃ plants was very similar with maxima in the leaves of ca 40 μmol NO₂ ^- g^-1 DW h^-1. ‘Basal’ NRA levels in shoot tissues of NH₄ ⁺ plants appeared relatively high with maxima in the leaves of ca 20 μmol NO₂ ^- g^-1 DW h^-1. Carboxylate to organic N ratios, (C-A)/N_org, on a whole plant basis varied from 0.2 in NH₄ ⁺ plants to 0.9 in NO₃ ^- plants. After withdrawal of N, all accumulated NO₃ ^- and NH₄ ⁺ was assimilated into organic N and the organic N redistributed on a large scale. NRA rapidly declined to similar low levels, irrespective of previous N source. Shoot/root ratios of -N plants were 50–80% lower than those from +N plants. In comparison with +N, RGR of -N plants did not decline to a large extent, decreasing by only 15% in -NH₄ ⁺ plants due to very high initial organic-N contents. N-deprived plants all exhibited an excess cation over anion uptake (net proton efflux), and whole-plant (C-A)/N_org ratios increased to values around unity. Possible difficulties in interpreting the (C-A)/N_org ratio and NRA of plants in their natural habitats are briefly discussed.     

Interactive effect of salt (NaCl) and nitrogen form on growth, water relations and photosynthetic capacity of sunflower (Helianthus annum L.)

The effects of the ammonium (NH₄⁺) and nitrate (NO₃^-) forms of nitrogen and NaCl on the growth, water relations and photosynthesis performance of sunflower (Helianthus annuus L.) were examined under glasshouse conditions. Eight-day-old plants of cv. Hisun 33 were subjected for 21 days to Hoagland's nutrient solution containing 8 mol m^-3N as NH₄⁺or NO₃^-, and salinised with 0, 60, or 120 mol m^-3NaCl. Fresh weights of shoots and roots, and leaf area of NO₃^-supplied non-salinised plants were significantly greater than those of NH₄⁺-supplied non-salinised plants. But addition of NaCl to the rooting medium of these plants had more inhibitory effect on the growth of NO₃^--supplied plants than on NH₄⁺-supplied plants. Both leaf water and osmotic potentials of plants grown with NH₄⁺were lower than those of plants given NO₃^-under both non-saline and saline conditions. Chlorophylls a and b concentrations were higher in plants grown with NH₄⁺than N0₃^--supplied plants at the lower two levels of salinisation. The rate of photosynthesis in plants was considerably higher in non-salinised plants grown with NO₃^-than with NH₄⁺, but with increase in salinisation the photosynthesis rate decreased in NO₃^--supplied plants, but not in those given NH₄⁺. The rate of transpiration was increased significantly by salinisation in NO₃^--supplied plants, but not consistently so in NH₄⁺-supplied plants. The stomatal conductances were much higher in plants given NO₃^-than with NH₄⁺when grown under non-saline conditions, but not when salinised. As a consequence, water-use efficiency in NO₃^--supplied control plants was better than in NH₄⁺-supplied under non-saline conditions, but worse under saline conditions. The different forms of nitrogen and the addition of NaCl to the growing medium did not affect the relative intercellular concentrations of CO₂ (C_i/C_a). Overall, the NH₄⁺form of nitrogen inhibited the growth of sunflowers under non-saline conditions, but NO₃^-and NaCl interacted to inhibit growth more than did NH₄⁺under saline conditions.     

Microphytobenthos activity and fluxes at the sediment-water interface: interactions and spatial variability

In this study oxygen and nutrient fluxes and denitrification rates across the sediment-water interface were measured via intact core incubations with a twofold aim: show whether microphytobenthos activity affects these processes and analyse the dispersion of replicate measurements. Eighteen intact sediment cores (i.d. 8 cm) were randomly sampled from a shallow microtidal brackish pond at Tjarno, on the west coast of Sweden, and were incubated in light and in darkness simulating in situ conditions. During incubation O₂, inorganic N and SiO₂ fluxes and denitrification rates (isotope pairing) were measured. Assuming mean values of 18 cores as best estimate of true average (BEA), the accuracy of O₂, NH₄ ⁺, NO₃ ^- and SiO₂ fluxes calculated for an increasing number of subsamples was tested. At the investigated site, microalgae strongly influenced benthic O₂, inorganic N and SiO₂ fluxes and coupled (D_n) and uncoupled (D_w) denitrification through their photosynthetic activity. In the shift between dark and light conditions NH₄ ⁺ and SiO₂ effluxes (60 and 110 µmol m^-2h^-1) and D_n (5 µmol m^-2 h^-1) dropped to zero, NO₃ ^- uptake (70 µmol m^-2 h^-1) showed a 30% increase, while D_w (20 µmol m^-2 h^-1) showed an 80% decrease. For O₂ and NO₃ ^- dark fluxes, 4 core replicates were sufficient to obtain averages within 5-10% of the best estimated mean, while 10-20% accuracy was obtained with 4-12 replicates for SiO₂ and >10 replicates for NH₄ ⁺ dark fluxes. Mean accuracy was considerably lower for all light incubations, probably due to the patchy distribution of the benthic microalgal community.     

Isolation and characterization of anthocyanin 5-O-glucosyltransferase from flowers of Dahlia variabilis

In the cyanic flowers ofDahlia variabilis (Asteraceae), an enzyme was demonstrated which catalyzes a glucosyl group transfer from UDP-glucose to the 5 position of anthocyanidin 3-O-glucoside and 3-O-malonylglucoside. The anthocyanin 5-O-glucosyltransferase (5GT) was purified 88-fold at 8 percnt; yield by (NH₄)₂SO₄ precipitation followed by successive chromatography on DEAE-cellulose, Sephacryl S-200 and Mono P. 5GT exhibited a pH optimum at 8.0 and a pI of 4. 2. Its apparent molecular weight calculated from Sephacryl S-200 was 53 kDa. Its activity was stimulated by 2-ME and DTE but strongly inhibited by PCMB and NEM. It was slightly activated by Mg²⁺ and Ca²⁺ but strongly inhibited by Hg²⁺, Zn²⁺, Cu²⁺, Mn²⁺, Fe³⁺ and Al³⁺. No effect of EDTA was observed. The apparent Km values for cyanidin 3-O-glucoside, cyanidin 3-O-(6′′-O-malonyl)glucoside and UDP-glucose were 120 μmol/L, 75 μmol/L and 250 μmol/L, respectively. Pelargonidin 3-O-glucoside and malonylglucoside were also considerable substrates, but low relative activity was observed for delphinidin 3-O-glucoside which has yet not been found inDahlia flowers.Dahlia 5GT showed substrate specificities different from those reported forSilene, Petunia, Matthiola andPerilla. Neither ADP-glucose nor UDP-galactose could serve as glycosyl donor.     

广州大夫山雨季林内外空气TSP和PM2.5浓度及水溶性离子特征

采用平行同步采样法,于2012年雨季,对广州市大夫山森林公园林内外空气的总悬浮颗粒物(TSP)和细颗粒物(PM_2.5)样品进行了24 h收集,测定了TSP和PM_2.5的质量浓度并分析了样品中水溶性无机离子成分。结果表明:林内外PM_2.5的质量浓度平均值分别为(40.18±10.47)和(55.79±13.01) g/cm³;林内外TSP的质量浓度分别为(101.32 ± 33.19)和(116.61±35.36) g/cm³。林内与林外比,PM_2.5和TSP平均质量浓度都显著减少(P < 0.05),表明森林能显著改善空气环境质量。TSP和PM_2.5中SO₄^2-、Na⁺、NH₄⁺和NO₃^-为水溶性无机离子主要成分,占总离子质量的80%以上,林外这些离子的浓度高于林内(NH₄⁺除外)。这4种离子雨季在空气中的主要存在方式为NaCl、Na₂SO₄、NH₄HSO₄和NH₄NO₃。计算表明,采样期间海盐对大夫山空气TSP和PM_2.5的水溶性组分中Na⁺和Cl^-贡献最大,其它元素主要源自陆地源。林内外TSP和PM_2.5的c(NO₃^-)/c(SO₄^2-)比值在0.3以下,表明固定源是大夫山森林公园空气主要污染贡献者,TSP中c(NO₃^-)/c(SO₄^2-)的比值大于PM_2.5的比值,说明移动源对TSP的贡献大于PM_2.5。     

Effect of nickel on certain physiological and biochemical behaviors of an acid tolerantChlorella vulgaris

This study concerns the inhibitory effects of acid pH and nickel on growth, nutrient (NO₃ ^- and NH₄ ⁺) uptake, carbon fixation, O₂ evolution, electron transport chain and enzyme (nitrate reductase and ATPase) activities of acid tolerant and wild-type strains of Chlorella vulgaris. Though a general reduction in all these variables was noticed with decreasing pH, the tolerant strain was found to be metabolically more active than the wild-type. A reduced cation (NH₄ ⁺, Na⁺, K⁺ and Ca²⁺) uptake, coupled with a facilitated influx of anions (NH₄ ⁺, PO₄ ^3- and HCO₃ ^-), suggested the development of a positive membrane potential in acid tolerant Chlorella. Nevertheless, a tremendous increase in ATPase activity at decreasing pH revealed the involvement of superactive ATPase in exporting H⁺ ions and keeping the internal pH neutral. A difference in Na⁺ and K⁺ efflux of the two strains at decreasing pH suggests there is a difference in membrane permeability. The low toxicity of Ni in the acid tolerant strain may be due to the low Ni uptake brought about by a change in membrane potential as well as in permeability. Hence, the development of superactive ATPase and a change in both membrane potential and permeability not only offers protection against acidity, but also co-tolerance to metals.     

Hydrogen peroxide is required for abscisic acid-induced NH4+ accumulation in rice leaves

The role of H₂O₂ in abscisic acid (ABA)-induced NH₄⁺ accumulation in rice leaves was investigated. ABA treatment resulted in an accumulation of NH₄⁺ in rice leaves, which was preceded by a decrease in the activity of glutamine synthetase (GS) and an increase in the specific activities of protease and phenylalanine ammonia-lyase (PAL). GS, PAL, and protease seem to be the enzymes responsible for the accumulation of NH₄⁺ in ABA-treated rice leaves. Dimethylthiourea (DMTU), a chemical trap for H₂O₂, was observed to be effective in inhibiting ABA-induced accumulation of NH₄⁺ in rice leaves. Inhibitors of NADPH oxidase, diphenyleneiodonium chloride (DPI) and imidazole (IMD), and nitric oxide donor (N-tert-butyl-α-phenylnitrone, PBN), which have previously been shown to prevent ABA-induced increase in H₂O₂ contents in rice leaves, inhibited ABA-induced increase in the content of NH₄⁺. Similarly, the changes of enzymes responsible for NH₄⁺ accumulation induced by ABA were observed to be inhibited by DMTU, DPI, IMD, and PBN. Exogenous application of H₂O₂ was found to increase NH₄⁺ content, decrease GS activity, and increase protease and PAL-specific activities in rice leaves. Our results suggest that H₂O₂ is involved in ABA-induced NH₄⁺ accumulation in rice leaves.     

闽江河口湿地土壤CH4产生与氧化速率对外源氮、硫添加的响应

通过室内培养实验,研究了外源氮、硫添加对闽江河口湿地土壤CH_4产生/氧化速率以及土壤理化性质的短期影响。NH_4Cl(N1)和NH_4NO_3(N3)处理在各培养阶段均显著促进土壤CH_4产生速率(P0.05),较对照分别提高136.70%和136.55%;NH_4Cl+K_2SO_4(NS1)和NH_4NO_3+K_2SO_4(NS3)处理在培养第3、6、12、15和18天均显著促进了CH_4产生速率(P0.05)。KNO_3(N2)、K_2SO_4(S)处理在不同培养时间对CH_4产生速率影响均不显著(P0.05);KNO_3+K_2SO_4(NS2)处理除在第21天外(P0.05),其他时间影响均不显著(P0.05)。N2、N3、NS2和NS3处理均显著促进了土壤CH_4氧化速率(P0.05),平均CH4氧化速率较CK分别提高了145.30%、142.93%、139.48%和112.68%。整体而言,不同添加处理并没有显著改变湿地土壤CH_4产生/氧化速率的时间变化规律,各处理均表现为随培养时间先增加而后逐渐降低。短期培养结束后,土壤可溶性有机碳(DOC)、电导率、p H值在不同处理间均不存在显著差异(P0.05);土壤NH+4-N含量在N1、N3、NS1和NS3处理下,NO_3~--N含量在N2、N3、NS2和NS3处理下,SO_4~(2-)含量在S、NS1、NS2和NS3处理下均显著高于对照处理(P0.05)。相关分析显示,DOC、铵态氮(NH+4-N)和硝态氮(NO_3~--N)是氮、硫添加处理下影响闽江河口湿地土壤CH_4产生/氧化速率短期变化的主要控制因素。     

Anoxic degradation of biogenic debris in sediments of eutrophic subalpine Lake Bled (Slovenia)

Anoxic degradation of sedimentary biogenic debris using closed sediment incubation experiments was studied in eutrophic subalpine Lake Bled (NW Slovenia) which, for most of the year, has an anoxic hypolimnion. Production rates of dissolved inorganic carbon (DIC), NH₄ ⁺, PO₄ ^3- and dissolved Si, and reduction rates of SO₄ ^2- were measured and anoxic mineralization rates were modelled using G-model. The depth profiles indicated major mineralization of biogenic debris and SO₄ ^2- reduction near the sediment surface. A comparison between depth integrated anoxic mineralization rates and diffusive benthic fluxes of DIC, NH₄ ⁺ and PO₄ ^3- showed that the anoxic incubation experiments provide a good estimate of N degradation of biogenic debris. The contributions of SO₄ ^2- reduction and acetate fermentation in NH₄ ⁺ production are about 30 and 70%, respectively. The DIC production accounted for only 15% of DIC benthic flux, indicating that methanogenesis and oxidation of methane provides 80% of this flux. Only about 30% of PO₄ ^3- was released because phosphate precipitated in the closed incubation experiments. The depth integrated production of Si accounts for 70–80% of Si benthic fluxes indicating intense dissolution of biogenic Si in the surficial lake sediment.     

Efficiency of respiration and energy requirements of N assimilation in roots of Pisum sativum

The function of alternative path respiration in roots was investigated in pea plants (Pisum sativum L. cv. Rondo). Plants were grown in symbiosis with Rhizobium leguminosarum (strain PF2), completely dependent on N₂ fixation, or non-nodulated, receiving nitrate or ammonium at the same rate as N₂ was fixed in symbiosis. Under these conditions, relative growth rates of plants grown with N₂, NO^-₃ or NH⁺₄ were the same. This facilitated interpretation of the effect of the N source on the efficiency of root respiration, as determined by the relative activity of the non-phosphorylating alternative path. The ‘wasteful’ oxidation of carbohydrate via this pathway was defined as the glucose equivalent of the difference between the amounts of ATP (mol O₂)^-1 produced in cytochrome and alternative path respiration. ‘Wasteful’ carbohydrate oxidation maximally amounted to 4% (N₂), 15% (NO^-₃) and 25% (NH⁺₄) of the daily carbohydrate oxidation in the roots. It is concluded that the ‘wasteful’ oxidation of carbohydrate via the alternative path is of minor importance for the adaptation of root respiratory metabolism to different energy requirements of N assimilation. The total carbohydrate import by roots fixing N₂ was ca 60 and 30% higher than the import by roots assimilating NO^-₃ or NH⁺₄, respectively. Two factors are shown to account for these differences: the high carbohydrate cost of N₂ fixation, and the small contribution (30%) of the roots to NO^-₃ reduction by the plant. The high carbohydrate requirements of roots fixing N₂ were met by higher rates of photosynthesis as compared with plants utilizing NO^-₃ or NH⁺₄.     

Cutaneous ion exchange,and renal and extrarenal partitioning of acid and ammonia excretion in the larval tiger salamander,Ambystoma tigrinum,following ingestion of ammonium salts

Summary The skin/gills and the kidneys of aquatic amphibians are potential sites of acid-base regulation. The roles of these organs in acid-base balance were examined in larval Ambystoma tigrinum following gastric infusion of ammonium salts. A single dose of 1.75 mEq NH₄Cl·100 g^-1 produced a mixed acidosis by 1 h after gavage. By 8 h after ingestion, pH and HCO ₃ ^– had increased and PCO₂ had decreased as the animals recovered. A prolonged acidosis was developed in a second group by gavage of an initial dose (1.5 mEq·100 g^-1), followed by periodic maintenance doses (0.25 mEq·100 g^-1) to prolong the disturbance for 8 h. The magnitude of the acidosis during this period was similar to that seen at 1 h after ingestion in the time-course study. A third group of larvae were given NaCl as a control for salt loading, which induced a small but significant respiratory acidosis. Unidirectional fluxes of Na⁺ and Cl^- were examined during these serial ingestions. Salt loading inhibited the influx of the ingested ion. Na⁺ influx increased during the NH₄Cl-induced acidosis. A fourth group of larvae were used to partition acid and ammonia excretion between the skin and the kidneys. These animals were given (NH₄)₂SO₄ to allow re-examination of Cl^- flux rates under non-Cl^--loaded conditions. The ensuing acidosis had a reduced respiratory component and, therefore, pH did not decrease as much. Cl^- influx rates did decrease significantly under these conditions. In both control and acidotic conditions, the majority of the acid efflux was as ammonia and the skin was the primary site of acid excretion. However, both the skin and the kidneys increased total acid excretion, although the efflux across the skin showed a much greater increase. This suggests a primary role for the skin in acid-base regulation in aquatic amphibians.Abbreviations GFR glomerular filtration rate - PO₂ partial pressure of oxygen - PCO₂ partial pressure of carbon dioxide - SITS 4-acetamido-4-isothiocynanatostilbene-2,2-disulfonic acid - TA titratible acidity Present address: Department of Organismal Biology and Anatomy, University of Chicago, 1025 E. 57th St., Chicago, IL 60637, USA     

Nitrogen regulation of gibberellin biosynthesis in Gibberella fujikuroi

Summary In Gibberella fujikuroi, ammonium (NH₄ ⁺) interfered with the production of gibberellic acid (GA₃). Optimal production occurred at 19 mm (NH₄)₂SO₄ and the synthesis of GA₃ was reduced threefold in a medium with 38 mm (NH₄)₂SO₄. Using a resting cell system with mycelia previously grown on two concentrations (19 mm and 38 mm) of (NH₄)₂SO₄, it was found that NH₄ ⁺ depressed synthesis of the gibberellin-synthesizing enzymes. Furthermore, addition of NH₄ ⁺ to a producing system shut off gibberellin formation, indicating that the negative effect of NH₄ ⁺ ions is also due to inhibition of one or more enzymes in the gibberellin biosynthesis pathway. The onset of gibberellin biosynthesis in media with high (38 mm) and low (19 mm) concentrations of (NH₄)₂SO₄ was studied by addition of cycloheximide to batch cultures of various ages. Offprint requests to: B. Brückner     

Electrophysiological factors in the influence of nitrate and ammonium ions on calcium uptake and translocation in tomato plants

Abstract Tomato plants (Lycopersicon esculentum Mill. cv. San Marzano), grown in dilute nutrient solutions containing (in meq ˙ 1^-1) 0.5 NaNO₃, 0.5 NH₄NO₃ or 0.25 (NH₄)₂ SO₄ as the nitrogen source, were detopped for collection of xylem sap and measurement of trans-root electrical potentials. The plant parts and the xylem exudate were subsequently analysed for mineral content. The commonly observed effects of NH₄⁺ were noted, including reduction of calcium concentration in the xylem sap, and of calcium content in stems and leaves, compared with NO₃^-fed plants. This effect was attributed principally to the less negative trans-root electrical potential measured in NH₄⁺-fed plants, and the resultant reduction of inward driving force on passively moving divalent cations.     

The effects of ammonium sulphate deposition and root sinks on soil solution chemistry in coniferous forest soils

The effects of enhanced (NH_{4 2}SO₄deposition on soil solution cation and anion concentrations and annualionic fluxes were followed using a standardised experimental protocolin six European coniferous forests with contrasting soil types, pollutioninputs and climate. Native soil cores containing a ceramic suction cupwere installed in the field, roofed and watered every two weeks withlocal throughfall or local throughfall with added(NH₄)₂SO₄ at 75 kgNH₄ ⁺-N ha^-1 a^-1. Livingroot systems were established in half of the lysimeters.Untreated throughfall NH₄ ⁺-N deposition at thesites ranged from 3.7 to 29 kg ha^-1 a^-1Soil leachates were collected at two weekly intervalsover 12 months and analysed for volume, andconcentrations of major anions and cations. Increasesin soil solution NO₃ ^- concentrations inresponse to N additions were observed after 4–9months at three sites, whilst one sandy soil with highC:N ratio failed to nitrify under any of thetreatments. Changes in NO₃ ^- concentrationsin soil solution controlled soil solution cationconcentrations in the five nitrifying soils, withAl³⁺ being the dominant cation in the more acidsoils with low base saturation. The acidification responses ofthe soils to the (NH_{4 2}SO₄additions were primarily related to the ability of thesoils to nitrify the added NH₄ ⁺. pH and soiltexture seemed important in controllingNH₄ ⁺ leaching in response to the treatments,with two less acidic, clay/clay loam sites showingalmost total retention of added NH₄ ⁺, whilstnearly 75% of the added N was leached asNH₄ ⁺ at the acid sandy soils. The presenceof living roots significantly reduced soil solutionNO₃ ^- and associated cation concentrations attwo of the six sites. The very different responses of the sixsoils to increased (NH₄)₂SO₄deposition emphasise that the establishment of N critical loadsfor forest soils need to allow for differences in N storagecapacity and nitrification potential.     

Dissolved oxygen and nutrient budgets in a phytotreatment pond colonised by <Emphasis Type="Italic">Ulva</Emphasis> spp.

Net daily budgets of dissolved oxygen (O₂), dissolved inorganic carbon (DIC), dissolved inorganic nitrogen (DIN = NH₄⁺+NO₂⁻+NO₃⁻) and soluble reactive phosphorus (SRP) were determined in a pond colonised by Ulva spp. This pond received wastewater from a land-based fish farm and was used as a phytotreatment plant. Three consecutive 24-h cycles of measurements were performed with 8–14 samplings per day. Water samples were collected at the inlet and outlet of the pond and budgets were estimated from differences between inlet and outlet loadings. The first cycle was started when Ulva biomass was 8 kg m⁻², as wet weight. The second cycle was performed after the harvest of ~20% of the macroalgal biomass and the third after the harvest of another ~20% of the remaining biomass. Ulva removal was very fast (<1 h) and samplings for cycles 2 and 3 were started two hours after harvesting, so that the whole experiment lasted ~80 h. When Ulva biomass was at its maximum, the aquatic system was heterotrophic with an O₂ demand of 519 mol d⁻¹ and a net regeneration of DIC (2686 mol d⁻¹), NH₄⁺ (49 mol d⁻¹) and SRP (2.5 mol d⁻¹). The DIC to O₂ ratio was an indicator of persistent anaerobic metabolism. Following the first harvest intervention, this system displayed a prompt response and shifted toward a lower O₂ demand (from −519 to −13 mol d⁻¹), with a lesser regeneration degree of NH₄⁺ (11.4 mol d⁻¹) and DIC (1066 mol d⁻¹). After the second Ulva removal the net budget of SRP became negative (−1.0 mol d⁻¹). By integrating these results over the three days cycle we estimated that in order to operate an efficient nutrient control and maintain macroalgal mats in a healthy status the optimal Ulva biomass should be well below ~4 kg m⁻² as wet weight. Above this threshold, self-limitation would render most of the algal mat unable to exploit light and nutrients. An efficient removal of nitrogen and phosphorus could be attained through the management of macroalgal biomass only with an optimisation of recipient surface to nutrient loading ratio.     

Simultaneous Study of NH+ 4, Na+, Mg2+, Ca2+, NO2- 3, SO2- 4, (NO- 2), H{2in}PO- 4 and CI- Uptake by Intact Winter Wheat Seedlings in a Single Depletion ExperimentPO- 4 and CI- Uptake by Intact Winter Wheat Seedlings in a Single Depletion Experiment

Simultaneous uptake of NH⁺ ₄, Na⁺, Mg²⁺, Ca²⁺, NO^- ₃, SO^2- ₄, (NO^- ₂), H²PO^- ₄ and C1^- ions by N-limited winter wheat seedlings(Triticum aestivum L., cv. Regina) in a single depletion experiment was investigated. Individual ion species in uptake solution samples were determined using capillary isotachophoresis. The operating systems used are described in detail. Processing of obtained concentration data allow to construct time curves of individual ions concentration in uptake solution, time curves of accumulative uptake, and curves for uptake rate versus time and uptake rate versus external concentration. From these curves there is possible to reveal a more complex picture of behaviour of individual ions during uptake process as well as to assess interactions among them. Attention was paid to the points of intersection of time curves of NO^- ₃ and NH⁺ ₄ uptake rates. These points characterized by equal uptake rates may be considered as limits for preference of given ion species under given experimental conditions.     

Mannitol Biosynthesis in Pyrenochaeta terrestris I. D-Maunitol-1-Phosphate: NAD Oxidoreductase

Cell-free extracts of mycelial mats of Pgrenochaeta terrestris grown in stationary culture on synthetic glucose or sucrose - salts liquid media contained D-mannitol-1-Phosphate:NAD oxidoreductase (EC 1.1.1.17) activity. Greatest activity occurred early in the growth period. The optimum pH for the reduction of NAD⁺ in the presence of Fru-6-P was 7.4–7.5 while the optimum pH for the oxidation of NADH in the presence of Mtl-1-P was 8.1–8.2. The enzyme was stabilized to some extent in Tris-maleate buffer, pH 7.5, and by the addition of 10% (NH₄)₂SO₄, to this buffer. A 10- to 16-fold purification was attained by a combination of (NH₄)₂SO₄ fractionation and gel filtration on Sephadex G-100. The enzyme was relatively specific in its substrate and coenzyme requirements. The Km values were determined as: Fru-6-P - 3 × 10^?4 M, Mtl-1-P - 1 × 10^?4 M, and NAD⁺ and NADH - 3 × 10^?5 M.     

Dissolved Nitrogen Uptake by a Cyanobacterial Bloom (Anabaena flos-aquae) in a Subarctic Lake

Uptake of dissolved nitrogen (NH₄⁺ + NO₃^- + urea + N₂) by a cyanobacterial [Anabaena flos-aquae (Lyngb.)] De Brèb population in Smith Lake, Alaska, was measured every 2 to 4 days during the spring of 1990. Total dissolved nitrogen uptake ranged from 0.34 to 24.75 μmol liter^-1 h^-1, with a mean of 5.75 μmol liter^-1 h^-1; the euphotic zone accounted for 91% of the uptake. The mean turnover time for dissolved combined nitrogen (NH₄⁺ + NO₃^- + urea) in the euphotic zone was less than 14 h, and that for NH₄⁺ was only 3.6 h. The mean relative preference indices for NH₄⁺ (2.4), NO₃^- (0.4), and urea (0.5) established NH₄⁺ as the preferred nitrogenous nutrient. The uptake rates were apparently dependent on biomass, temperature, and light. Regeneration, probably due to zooplankton excretion and bacterial remineralization of dissolved organic nitrogen, was the main source of NH₄⁺ for the cyanobacterial growth. The high half-saturation constant for NH₄⁺ with low ambient NH₄⁺ concentration nevertheless resulted in the simultaneous utilization of several forms of nitrogen.