Ammonia,tetraethylammonium, barium and amiloride induce metamorphosis in the marine hydroid Hydractinia

Summary In Hydractinia metamorphosis from the swimming larval stage to the sessile polyp stage has been found to be inducible by several agents, including Li⁺, K⁺, Cs⁺, Rb⁺, diacylglycerol (DG), tetradecanoyl-phorbol-acetate (TPA) and some other tumour-promoting phorbol esters. Induction is antagonized by ouabain and compounds which are able to increase the internal level of S-adenosylmethionine (SAM). Based on the finding that Hydractinia larvae contain such compounds in a stored form, including N-methylpicolinic acid, N-methylnicotinic acid and N-trimethylglycine, as well as on the results of experiments with antagonists of SAM production and transmethylation, it has been argued that regulation of the internal SAM level plays a key role in the control of metamorphosis. However, it remains to be clarified whether the inducing agents act by decreasing the SAM level or by via different pathways. In the present study, substances chemically related to the substances known to induce or inhibit metamorphosis were tested for their metamorphosis-inducing abilities. Some were found to be effective, including NH₄ ⁺, methylamine, tetraethylammonium ions (TEA⁺), ethanolamine, Ba²⁺, Sr²⁺ and the diuretic, amiloride. It is of particular interest that in many organisms TPA and DG increase cytoplasmic pH while amiloride prevents a rise in pH_i. Several of the substances known to trigger metamorphosis may increase the internal NH₄ ⁺ concentration by hindering the export of the constantly produced NH₄ ⁺ through K⁺ channels or through the Na⁺-H⁺ antiport. Treatment with Cs⁺ for 1 h increases the internal level of NH₄ ⁺. Produced and applied ammonia, as well as applied methylamine and ethanolamine, may act by accepting methyl groups, thus reducing the SAM level.     

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.     

Nitrogen limitation in mycorrhizal Norway spruce (Picea abies) seedlings induced mycelial foraging for ammonium: implications for Ca and Mg uptake

Although many studies support the importance of the external mycelium for nutrient acquisition of ectomycorrhizal plants, direct evidence for a significant contribution to host nitrogen nutrition is still scarce. We grew nonmycorrhizal seedlings and seedlings mycorrhizal with Paxillus involutus (Batsch) Fr. in a sand culture system with two compartments separated by a 45-m Nylon mesh. Hyphae, but not roots, can penetrate this net. Nutrient solutions were designed to limit seedling growth by nitrogen. Hyphal density in the hyphal compartment, host N status and shoot growth of mycorrhizal seedlings significantly increased in response to NH₄ ⁺ addition to the hyphal compartment. Labeling the compartment only accessible to hyphae with ¹⁵NH₄ ⁺ showed that the increase in N uptake in the mycorrhizal seedlings was a result of hyphal N acquisition from the hyphal compartment. These results indicate that hyphae of P. involutus may actively forage into N-rich patches and improve host N status and growth. In the mycorrhizal seedlings, which received additional NH₄ ⁺ via their external mycelium, the increase in NH₄ ⁺ supply less negatively affected Ca and Mg uptake than in nonmycorrhizal seedlings, where the additional NH₄ ⁺ was directly supplied to the roots. This was most likely due to the close link of NH₄ ⁺ uptake and H⁺ extrusion, which, in the nonmycorrhizal seedlings, lead to a strong acidification in the root compartment, and subsequently reduced Ca and Mg uptake, whereas in the mycorrhizal seedlings the site of intensive NH₄ ⁺ uptake and acidification was in the hyphal and not in the root compartment. Our data support the idea that the ectomycorrhizal mycelium connected to an N-deficient host may actively forage for N. The mycelium may also be important as a biological buffer system ameliorating negative influence of high NH₄ ⁺ supply on cation uptake.     

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.     

Intracellular measurement of ammonium in Chara corallina using ion-selective microelectrodes

The study of ammonium (NH₄ ⁺) transport across plant cell membranes requires accurate measurement of NH₄ ⁺ gradients across subcellular gradients. We have developed an ammonium-selective microelectrode based on the ionophore nonactin. This electrode can detect NH₄ ⁺ activities (a_NH4) in vivo in the millimolar range in the presence of cytosolic levels of potassium, the main interfering ion. The electrode was used to measure intracellular a_NH4 in internodal cells of the giant alga Chara corallina. Results from cells incubated in media supplemented with 1 mM NH₄ ⁺ produced two populations, with means of 7.3 and 30.8 mM, respectively. HPLC analysis of vacuolar sap suggests the higher population represents vacuolar impalements, and the lower population can thus be assumed to be cytosolic. These results suggest a four-fold accumulation of NH₄ ⁺ in the vacuolar compartment of Chara. This revised version was published online in June 2006 with corrections to the Cover Date.     

The influence of NO3 - and NH4 + nutrition on the carbon and nitrogen partitioning characteristics of wheat (Triticum aestivum L.) and maize (Zea mays L.) plants

The carbon and nitrogen partitioning characteristics of wheat (Triticum aestivum L.) and maize (Zea mays L.) grown hydroponically at a constant pH on either 4 mM or 12 mM NO₃ ^- or NH₄ ⁺ nutrition were investigated using either ¹⁴C or ¹⁵N techniques. Greater allocation of ¹⁴C to amino-N fractions occurred at the expense of allocation of ¹⁴C to carbohydrate fractions in NH₄ ⁺-compared to NO₃ ^--fed plants. The [¹⁴C]carbohydrate:[¹⁴C]amino-N ratios were 1.5-fold and 2.0-fold greater in shoots and roots respectively of 12 mM NO₃ ^--compared to 12 mM NH₄ ⁺-fed wheat. In both 4 mM and 12 mM N-fed maize the [¹⁴C]carbohydrate:[¹⁴C]amino-N ratios were approximately 1.7-fold and 2.0-fold greater in shoots and roots respectively of NO₃ ^--compared to NH₄ ⁺-fed plants. Similar results were observed in roots of wheat and maize grown in split-root culture with one root-half in NO₃ ^--and the other in NH₄ ⁺-containing nutrient media. Thus the allocation of carbon to the amino-N fractions occurred at the expense of carbohydrate fractions, particularly within the root. Allocation of ¹⁴N and ¹⁵N within separate sets of plants confirmed that NH₄ ^--fed plants accumulated more amino-N compounds than NO₃ ^--fed plants. Wheat roots supplied with ¹⁵NH₄ ⁺ for 8 h were found to accumulate ¹⁵NH₄ ⁺ (8.5 g ¹⁵N g^-1 h^-1) whereas in maize roots very little ¹⁵NH₄ ⁺ accumulated (1.5 g ¹⁵N g^-1 h^-1)It is proposed that the observed accumulation of ¹⁵NH₄ ⁺ in wheat roots in these experiments is the result of limited availability of carbon within the roots of the wheat plants for the detoxification of NH₄ ⁺, in contrast to the situation in maize. Higher photosynthetic capacity and lower shoot: root ratios of the C₄ maize plants ensure greater carbon availability to the root than in the C₃ wheat plants. These differences in carbon and nitrogen partitioning between NO₃ ^--and NH₄ ⁺-fed wheat and maize could be responsible for different responses of wheat and maize root growth to NO₃ ^- and NH₄ ⁺ nutrition.     

Ammonium ion, ethylene, and NaCl-induced senescence of detached rice leaves

The possibility that NH₄ ⁺ accumulation is linkedto the senescence of detached rice (Oryza sativa) leavesinduced by NaCl was investigated. NaCl was effective in promoting senescenceandin increasing NH₄ ⁺ content of detached rice leaves.NaCl-promoted senescence is mainly due to the effect of both Na⁺ andCl^- ions. NaCl had no or slight effect on relative water content,suggesting that an osmotic effect is unlikely to be a major factor contributingto senescence of these leaves. NaCl-induced NH₄ ⁺accumulation was due to enhanced nitrate reduction and decreased glutaminesynthetase activity. Exogenous NH₄Cl, which caused an accumulationofNH₄ ⁺ in detached rice leaves, also promoted senescence.Itwas found that an increase in NH₄ ⁺ content preceded theoccurrence of senescence caused by NaCl. Results also show that NaCl-promotedsenescence is unlikely to be due to the lack of glutamate, glutamine,aspartate,and asparagine. The current results suggest that NH₄ ⁺accumulation is linked to NaCl-induced rice leaf senescence. Since ethylene isknown to be a potent promoter of leaf senescence, we also investigated the roleof ethylene in the regulation of NH₄ ⁺-promoted senescenceof detached rice leaves. NaCl or NH₄Cl treatment resulted in adecrease of ethylene production. Evidence was presented to show thatNH₄ ⁺ accumulation in detached rice leaves does not changetissue sensitivity to ethylene. Clearly, the possible involvement of ethyleneinNH₄ ⁺-promoted senescence is excluded.     

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。     

Some properties of a Klebsiella pneumoniae ammonium transport negative mutant (Amt−)

The main property of an Amt^- (ammonium transport negative) mutant of Klebsiella pneumoniae is its inability to accumulate NH ₄ ⁺ intracellularly. When growing on nitrogen sources other than NH ₄ ⁺ , the mutant constantly looses NH₃ by diffusion. This loss results in poor growth. The NH₃ excretion suggests the existence of a futile cycle (NH₃ loss/NH ₄ ⁺ reabsorption) in the wild type and possibly other bacterial strains, which do not constantly excrete NH₃.Dedicated to Prof. R. H. Burris     

双功能尿苷酰转移/去除酶GlnD在谷氨酸棒杆菌JNR中的功能

【目的】通过改造谷氨酸棒杆菌JNR中双功能尿苷酰转移/去除酶GlnD,减弱尿苷酰去除酶的活性,增强NH_4~+的转运和利用,提高L-精氨酸的合成。【方法】本文对来源于谷氨酸棒杆菌的突变菌株JNR中的双功能尿苷酰转移/去除酶GlnD进行整合突变,采用同源重组的方法将H_(414)和D_(415)位点突变为两个丙氨酸AA,在此菌株的基础上过量表达PII蛋白GlnK,并对其进行尿苷酰化研究,离子色谱检测摇瓶发酵过程中NH4+的浓度,并对最终的改造菌株进行连续流加发酵分析。【结果】该双功能尿苷酰转移/去除酶在谷氨酸棒杆菌中成功进行整合突变,有效减弱了尿苷酰去除酶的活性;同时过表达PII蛋白GlnK,其酰基化程度明显增强。摇瓶发酵结果表明菌株L4消耗NH_4~+增加,L-精氨酸产量为36.2±1.2 g/L,比对照菌株L3高出22.7%。5-L发酵罐实验结果显示改造菌株L4的L-精氨酸的产量为52.2 g/L,较野生型菌株L0提高了25.3%。【结论】谷氨酸棒杆菌合成L-精氨酸的过程中氮源是必不可少的。减弱GlnD尿苷酰去除酶的活性后,胞内尿苷酰化的GlnK-UMP增加,GlnK-UMP与氮转录调控因子AmtR结合,转运至胞内的NH_4~+浓度提高,促使L-精氨酸产量显著提高。     

Enhancing yield of <Emphasis Type="Italic">S</Emphasis>-adenosylmethionine in <Emphasis Type="Italic">Pichia pastoris</Emphasis> by controlling NH<Subscript>4</Subscript><Superscript>+</Superscript> concentration

Yield of S-adenosylmethionine was improved significantly in recombinant Pichia pastoris by controlling NH₄ ⁺ concentration. The highest production rate was 0.248 g/L h when NH₄ ⁺ concentration was 450 mmol/L and no repression of cell growth was observed. Within very short induction time (47 h), 11.63 g/L SAM was obtained in a 3.7 L bioreactor.     

Growth and solute composition of the salt-tolerant kallar grass [Leptochloa fusca (L.) Kunth] as affected by nitrogen source

A study was conducted to elucidate the effect of N form, either NH₄ ⁺ or NO₃ ^–, on growth and solute composition of the salt-tolerant kallar grass [Leptochloa fusca (L.) Kunth] grown under 10 mM or 100 mM NaCl in hydroponics. Shoot biomass was not affected by N form, whereas NH₄ ⁺ compared to NO₃ ^– nutrition caused an almost 4-fold reduction in the root biomass at both salinity levels. Under NH₄ ⁺ nutrition, salinity had no effect on the biomass yield, whereas under NO₃ ^– nutrition, increasing salinity from 10 mM to 100 mM caused 23% and 36% reduction in the root and shoot biomass, respectively. The reduced root growth under NH₄ ⁺ nutrition was not attributable to impaired shoot to root C allocation since N form did not affect the overall root sugar concentration and the starch concentration was even higher under NH₄ ⁺ compared to NO₃ ^– nutrition. The low NH₄ ⁺ (2 mM) and generally higher amino-N concentrations in NH₄ ⁺- compared to NO₃ ^–-fed plants indicated that the grass was able to effectively detoxify NH₄ ⁺. Salinity had no effect on Ca²⁺ and Mg²⁺ levels, whereas their concentration in shoots was lower under NH₄ ⁺ compared to NO₃ ^– nutrition (over 66% reduction in Ca²⁺; over 20% reduction in Mg²⁺), but without showing deficiency symptoms. Ammonium compared to NO₃ ^– nutrition did not inhibit K⁺ uptake, and the K⁺-Na⁺ selectivity either remained unaffected or it was higher under NH₄ ⁺ than under NO₃ ^– nutrition. Results suggested that while NH₄ ⁺ versus NO₃ ^– nutrition substantially reduced root growth, and also strongly modified anion concentrations and to a minor extent concentrations of divalent cations in shoots, it did not influence salt tolerance of kallar grass.     

Effect of phosphinothricin (glufosinate) on photosynthesis and photorespiration of C3 and C4 plants

Phosphinothricin (glufosinate), an irreversible inhibitor of glutamine synthetase, causes an inhibition of photosynthesis in C₃ (Sinapis alba) and C₄ (Zea mays) plants under atmospheric conditions (400 ppm CO₂, 21% O₂). This photosynthesis inhibition is proceeding slower in C₄ leaves. Under non-photorespiratory conditions (1000 ppm CO₂, 2% O₂) there is no inhibition of photosynthesis. The inhibition of glutamine synthetase by phosphinothricin results in an accumulation of NH₄ ⁺. The NH₄ ⁺-accumulation is lower in C₄ plants than in C₃ plants. The inhibition of glutamine synthetase through phosphinothricin in mustard leaves results in a decrease in glutamine, glutamate, aspartate, asparagine, serine, and glycine. In contrast to this, a considerable increase in leucine and valine following phosphinothricin treatment is measured. With the addition of either glutamine, glutamate, aspartate, glycine or serine, photosynthesis inhibition by phosphinothricin can be reduced, although the NH₄ ⁺-accumulation is greatly increased. This indicates that NH₄ ⁺-accumulation cannot be the primary cause for photosynthesis inhibition by phosphinothricin. The investigations demonstrate the inhibition of transmination of glyoxylate to glycine in photorespiration through the total lack of amino donors. This could result in a glyoxylate accumulation inhibiting ribulose-1,5-bisphosphate-carboxylase and consequently CO₂-fixation.Abbreviations GOGAT glutamine-2-oxoglutarate-amidotransferase - GS glutamine synthetase - PPT phosphinothricin - MSO methionine sulfoximine - RuBP ribulose-1,5-bisphosphate     

Ammonia production from yeast extract and its effect on growth of the hyperthermophilic archaeonSulfolobus solfataricus

Utilization of yeast extract and formation of byproduct metabolite were investigated for hyperthermophilic archaeonSulfolobus solfataricus (DSM 1617). In both batch and fed-batch cultivations ofS. solfataricus, maximal cell density, NH₄ ⁺ ion production and pH change were highly dependent on the ratio of yeast extract to glucose in the medium. Variation of NH₄ ⁺ ion level was identified as a major cause of pH change during cultivation, and acidification of culture broth was attributed to consumption of NH₄ ⁺ ions rather than formation of acid byproducts. It was also observed that increase of NH₄ ⁺ ion concentrations in the medium resulted in greater degree of growth inhibition.     

The kinetics of NH4 + and NO3 − uptake by Douglas fir from single N-solutions and from solutions containing both NH4 + and NO3 −

The kinetics of NH₄ ⁺ and NO₃ ⁻ uptake in young Douglas fir trees (Pseudotsuga menziesii [Mirb.] Franco) were studied in solutions, containing either one or both N species. Using solutions containing a single N species, the V_max of NH₄ ⁺ uptake was higher than that of NO₃ ⁻ uptake. The K_m of NH₄ ⁺ uptake and K_m of NO₃ ⁻ uptake differed not significantly. When both NH₄ ⁺ and NO₃ ⁻ were present, the V_max for NH₄ ⁺ uptake became slightly higher, and the K_m for NH₄ ⁺ uptake remained in the same order. Under these conditions the NO₃ ⁻ uptake was almost totally inhibited over the whole range of concentrations used (10–1000 μM total N). This inhibition by NH₄ ⁺ occurred during the first two hours after addition. ei]{gnA C}{fnBorstlap}     

The effect of copper toxicity on the contents of nitrogen compounds in Silene vulgaris (Moench) Garcke

The effect of copper on the uptake of nitrogen and the tissue contents of inorganic nitrogen, amino acids and proteins were studied in cooper-sensitive Silene vulgaris (Moench) Garcke, grown at different nitrogen sources (NH₄ ⁺ or NO₃ ^-). All the toxic copper levels tested, i.e. 4, 8, 16 M Cu²⁺, strongly inhibited the uptake of nitrogen, especially of NO₃ ^-, and decreased the content of NO₃ ^-, amino acids and proteins. Especially at 4 and 8 M Cu²⁺, NH₄ ⁺ accumulated in the plants, suggesting that the conversion of NH₄ ^- into amino acids was inhibited.     

Shewanella putrefaciens CN32对粘土附着态铵氮释放的影响

【目的】研究产胞外分泌物微生物Shewanella putrefaciens CN32对土壤中常见粘土矿物附着态NH_4~+的释放效果及影响机制。【方法】以吸附NH_4~+的蒙脱石、蛭石、伊蒙混层矿物和黑云母为对象,通过监测S. putrefaciens CN32作用下不同粘土释放的NH_4~+含量及过程,以及监测微生物量及释放的胞外聚合物(Extracellular Polymeric Substances,EPS)的含量变化,研究S. putrefaciens CN32作用下不同粘土矿物类型附着态NH_4~+释放的差异性。【结果】粘土矿物附着态NH_4~+含量从高到低依次为蒙脱石蛭石伊蒙混层矿物黑云母(黑云母NH_4~+吸附量极低,会在非生物作用下几乎完全释放),CN32作用下粘土附着态NH_4~+相对释放量依次为蒙脱石伊蒙混层矿物蛭石;然而,尽管CN32有效促进了粘土附着态NH_4~+释放,但释放的NH_4~+并未在溶液中大量累积,而是多被微生物同化吸收转化为生物有机氮(EPS为主)并吸附在粘土表面,且粘土对EPS的吸附能力表现为蒙脱石伊蒙混层矿物蛭石黑云母;由于粘土吸附NH_4~+及EPS都与矿物中的羟基(结构水或层间水)关系密切,推测EPS对矿物羟基的竞争吸附可能是CN32促进NH_4~+释放的重要原因之一。【结论】以上结果表明,产EPS微生物S. putrefaciens CN32能够促进各类粘土矿物的附着态NH_4~+释放,但释放的NH_4~+可以通过微生物作用转化为有机氮,从而在减少NH_4~+流失的同时增加土壤氮肥的生物可利用性,因此微生物在降低土壤氮肥流失、转化土壤氮肥污染过程中可能起到了重要作用,也揭示了深入系统地分析不同类型土壤(粘土类型不同)中粘土附着态NH_4~+在不同功能微生物作用下的迁移转化过程,是精准评估土壤氮肥施用效率及流失风险的前提之一。     

Regulation of NH4 + transport pathways in Pisum arvense roots

The effects of metabolic and protein synthesis inhibitors on NH₄ ⁺ uptake by Pisum arvense plants at low (0.05 mM) and high (1 mM) external ammonium concentration were studied. In short-time experiments cycloheximide decreased the ammonium uptake rate at low level of NH₄ ⁺ and increased the absorption of NH₄ ⁺ from uptake medium containing high ammonium concentration. Arsenate and azide supplied into uptake solutions at low ammonium concentration strongly decreased or completely suppressed the NH₄ ⁺ uptake rate, respectively. When the experiments were carried out at high level of ammonium only azide decreased the uptake rate of NH₄ ⁺ and arsenate stimulated this process. Dinitrophenol very strongly repressed the uptake rate of NH₄ ⁺ at both ammonium concentrations. After removing dinitrophenol from both solutions, neither at low nor high external ammonium level the recovery of NH₄ ⁺ uptake rate was achieved within 150 min or 3 h, respectively. The recovery of NH₄ ⁺ uptake rate after removing azide was observed within 90 min and 3 h at low and high ammonium concentrations, respectively. The regulation of NH₄ ⁺ uptake by some inhibitors at low external ammonium level was investigated using plasma membrane vesicles isolated from roots by two-phase partitioning. Orthovanadate completely suppressed the uptake of NH₄ ⁺ by vesicles and quinacrine decreased the NH₄ ⁺ uptake which 55 suggests that ammonium uptake depends on activities of plasma membrane-bound enzymes. On the other hand, it was found that dinitrophenol completely reduced the NH₄ ⁺ uptake by vesicles. The various effects of inhibitors on ammonium uptake dependent on external ammonium concentration suggest the action of different ammonium transport systems in Pisum arvense roots. The ammonium transport into root cells at low NH₄ ⁺ level requires energy and synthesis of protein in the cytoplasm. The research was supported by grant of KBN No. 6PO4C 068 08     

黑河天涝池流域典型林分生态水文化学特征

采集了黑河天涝池流域典型林分林外雨、穿透雨、树干径流和枯透水,并检测水体pH值和12种离子(K~+、Ca~(2+)、Na~+、Mg~(2+)、NH_4~+、Cu~(2+)、Zn~(2+)、Pb~(2+)、Cd~(2+)、Cl~-、SO_4~(2-)、NO_3~3)的质量浓度。结果表明:天涝池流域大气降水pH均值为7.74,呈碱性,降水中离子绝对质量浓度较低,最高的是NO_3~-,质量浓度为1.1111 mg/L,最低的为Na~+,质量浓度为0.0108 mg/L;两种林分冠层有降低降雨pH值的作用,青海云杉林冠层对NH_4~+有升高作用,祁连圆柏林冠层对NH_4~+有降低作用,两种林冠层对NO_3~-和Cu~(2+)质量浓度有降低作用,对其它离子质量浓度均表现为升高作用;两种林分树干径流有提高穿透雨pH值的作用,与穿透雨相比,两种林分树干径流中阴离子均有升高,圆柏树干径流中所有阳离子质量浓度均有下降,云杉树干径流中Ca~(2+)、K~+、Mg~(2+)和Na~+减少,NH_4~+和Cu~(2+)增加;典型林分枯透水有提升穿透雨pH值的作用,与穿透雨相比,两种林分枯透水中阴离子质量浓度均有升高,云杉枯透水各阳离子均有降低,圆柏枯透水中Ca~(2+)、K~+和Mg~(2+)质量浓度升高,NH_4~+、Na~+和Cu~(2+)质量浓度下降;在采集的所有样本中,Pb~(2+)和Cd~(2+)均未检出,而Zn~(2+)仅在云杉树干径流中检出。