Effects of pH on ammonium uptake by Typha latifolia L.

The effects of solution pH on NH₄⁺ uptake kinetics and net H⁺ extrusion by Typha latifolia L. were studied during short-term (days) and long-term (weeks) exposure to pH in the range of pH 3.5–8.0. The NH₄⁺ uptake kinetics were estimated from depletion curves using a modified Michaelis-Menten model. T. latifolia was able to grow in solution culture with NH₄⁺ as the sole N source and to withstand a low medium pH for short periods (days). With prolonged exposure (weeks) to pH 3.5, however, the plants showed severe symptoms of stress and stopped growing. The solution pH affected NH₄⁺ uptake kinetics. The affinity for NH₄⁺, as quantified by the half saturation constant (K_1/2) and C_min (the NH₄⁺ concentration at which uptake ceases), decreased with pH. K_1/2 was increased from 7.1 to 19.2 mmol m^?3 and C_min from 2.0 to 5.7 mmol m^?3 by lowering the pH in steps from 8.0 to 3.5. V_max was, however, largely unaffected by pH (～22 μmol h^?1 g^?1 root dry weight). Under prolonged exposure to constant pH, growth rates were highest at PH 5.0 and 6.5. At pH 8.0 growth was slightly depressed and at pH 3.5 growth completely stopped. NH₄⁺ uptake kinetics were similar at pH 5.0, 6.5 and 8.0 whereas at pH 3.5 NH₄⁺ uptake almost completely stopped. The ratio between net H⁺ extrusion and NH₄⁺ uptake decreased significantly at low pH. The adverse effects of low pH on NH₄⁺ uptake kinetics are probably a consequence of a reduced H⁺-ATPase activity and/or an increased re-entry of H⁺ at low pH, and the associated decrease in the electrochemical gradient across the plasma membranes of the root cells.     

Measuring Nitrogen and Phosphorus Uptake by Intact Roots of Mature Acer saccharum Marsh., Pinus resinosa Ait., and Picea abies (L.) Karst

A common method for measuring uptake by intact roots in situ is the depletion method, wherein intact fine roots are separated from soil and placed in nutrient solution. The difference between initial and final amounts of nutrient in solution is attributed to root uptake. Variations on this method include applying pretreatment solutions, training roots to grow into bags or trays, and varying concentrations of nutrient solution. We tested whether variations in methods affected measured net uptake rates of NH ₄ ⁺ , NO ₃ ⁻ , and PO ₄ ³⁻ . Intact roots of 60 year-old sugar maple (Acer saccharum Marsh.), red pine (Pinus resinosa Ait.), and Norway spruce (Picea abies (L.) Karst.) were given one of four treatments prior to measuring net uptake. “Trained” roots were grown in a sand-soil mixture. “Recovered” roots were excavated and allowed to recover in nutrient solution for two or four days (“two-day recovery” and “four-day recovery”, respectively). “No recovery” roots were excavated and used immediately in experiments. We exposed roots to three concentrations of nutrient solutions to observe the effects of initial nutrient solution concentration. Initial nutrient solution concentration was an important source of variation in measured uptake rates, and N uptake was stimulated by low antecedent concentrations. We found no significant differences in net uptake rates between pretreatments for any of the species studied, indicating that our pretreatments were not effective in improving measurement of uptake. Such pretreatments may not be necessary for measuring net uptake and may not hinder the comparison of rates measured using variations of the depletion method.     

NH4 + transport system of a psychrophilic marine bacterium, Vibrio sp. strain ABE-1

NH₄ ⁺ transport system of a psychrophilic marine bacterium Vibrio sp. strain ABE-1 (Vibrio ABE-1) was examined by measuring the uptake of [¹⁴C]methylammonium ion (¹⁴CH₃NH^{3 +}) into the intact cells. ¹⁴CH₃NH₃ ⁺ uptake was detected in cells grown in medium containing glutamate as the sole nitrogen source, but not in those grown in medium containing NH₄Cl instead of glutamate. Vibrio ABE-1 did not utilize CH₃NH₃ ⁺ as a carbon or nitrogen source. NH₄Cl and nonradiolabeled CH₃NH₃ ⁺ completely inhibited ¹⁴CH₃NH₃ ⁺ uptake. These results indicate that ¹⁴CH₃NH₃ ⁺ uptake in this bacterium is mediated via an NH₄ ⁺ transport system and not by a specific carrier for CH₃NH₃ ⁺. The respiratory substrate succinate was required to drive ¹⁴CH₃NH₃ ⁺ uptake and the uptake was completely inhibited by KCN, indicating that the uptake was energy dependent. The electrochemical potentials of H⁺ and/or Na⁺ across membranes were suggested to be the driving forces for the transport system because the ionophores carbonylcyanide m-chlorophenylhydrazone and monensin strongly inhibited uptake activities at pH 6.5 and 8.5, respectively. Furthermore, KCl activated ¹⁴CH₃NH₃ ⁺ uptake. The ¹⁴CH₃NH₃ ⁺ uptake activity of Vibrio ABE-1 was markedly high at temperatures between 0° and 15°C, and the apparent K _m value for CH₃NH₃ ⁺ of the uptake did not change significantly over the temperature range from 0° to 25°C. Thus, the NH₄ ⁺ transport system of this bacterium was highly active at low temperatures. Received: August 1, 1998 / Accepted: October 8, 1998     

不同营养条件下竹叶眼子菜NH4+-N吸收动力学的初步研究

以竹叶眼子菜(Potamogeton malaianus)无菌系种苗为试验材料,研究了不同水体营养浓度水平(低营养:TN0.213 mg·L^-1,TP 0.0093 mg·L^-1;中营养:TN 0.71 mg·L^-1,TP 0.031 mg·L^-1;高营养:TN 7.1 mg·L^-1,TP0.31 mg·L^-1)对其生长与NH₄⁺-N的吸收动力学参数的影响。结果表明,不同浓度水体营养对竹叶眼子菜生长的影响较小,而NH₄⁺-N的吸收动力学参数有显著差异。竹叶眼子菜在高、中和低营养培养条件下的NH₄⁺-N最大吸收速率V_max分别为41.1、29.1、21.1μmol·g^-1·h^-1,米氏常数K_m分别为0.356、0.306、0.122 mmol·L^-1。竹叶眼子菜营养吸收动力学与其生长环境关系紧密,在低浓度生长环境中时,竹叶眼子菜可以通过降低K_m值来提高对营养离子的亲和力以满足营养需求;在高浓度生长环境中,该植物通过增大吸收潜力来适应高营养。     

稻鸭共作生态系统稻田土壤固定态铵含量及有效性

通过田间试验研究了稻鸭共作生态系统土壤固定态铵的动态及有效性和温度、土壤pH、土壤交换性铵及土壤质地对土壤固定态铵的影响.研究结果表明:(1)在水稻生育期间,土壤固定态铵含量处于不断变化之中,施肥促进土壤对铵的固定,水稻的吸收促进土壤固定态铵的释放;其中在固定态铵释放过程之中,新固定的肥料铵几乎完全释放,而原有固定态铵没有释放.(2)较之常规稻作,稻鸭共作显著地提高了土壤固定态铵含量,其平均含量高出常规稻作的7%.(3)土壤交换性NH 4含量和pH与土壤固定态铵含量呈显著正相关(p<0.01);土壤温度(5cm土层)与土壤固定态铵含量间不相关;土壤固定态铵含量与>0.2mm的砂粒含量和<0.002mm的粘粒含量呈显著或极显著相关,而与0.02～0.2mm和0.002～0.02mm粘粒含量不相关.     

稻鸭共作对稻田氮素变化及土壤微生物的影响

通过田间试验研究稻鸭共作生态系统中土壤与田面水全N、无机N的动态变化及水稻吸N的规律和土壤微生物数量的变化规律.结果表明,(1)与常规稻作相比,稻鸭共作稻田土壤、田面水全N含量略有提高,土壤、田面水NH 4含量和水稻含N量显著提高,而土壤、田面水NO-3含量无明显变化;(2)稻鸭共作极显著提高了水稻总吸N量,高于常规稻作17.8%;相关分析显示,水稻吸N量与NH 4含量呈一元二次方程式关系,达到显著或极显著相关.(3)与常规稻作相比,稻鸭共作能显著提高土壤微生物数量,其中细菌数最多,放线菌次之,真菌最少.     

SHORT TERM UPTAKE OF NUTRIENTS BY ENTEROMORPHA PROLIFERA (CHLOROPHYCEAE)1

Rates of NH₄⁺ and NO₃^? uptake were determined by accumulation of ¹⁵N in plant tissue and by disappearance of nutrient from the medium. Agreement between rates calculated by the two methods was good, averaging 82.7% (SD = 15.8%) and 91.2% (SD = 13.7%) for NH₄⁺ and NO₃^? uptake, respectively. An average of 93.4 and 96.0% of added ¹⁵NH₄⁺ and ¹⁵NO₃^? was recovered from the medium and /or plant tissue at the end of the incubations. Both bacterial uptake and regeneration of NH₄⁺ may contribute to discrepancies between NH₄⁺ uptake rates calculated by ¹⁵N accumulation and disappearance of NH₄⁺ from the medium. The influence of tissue composition on uptake of NH₄⁺, NO₃^? and PO₄^3- by Enteromorpha prolifera (Müller) J. Agardh was examined. For NH₄⁺ uptake, V_max was 188 μmol NH₄^+. g dry wt^?1. h^?1 and K_s ranged from 9.3 to 13.4 μM, but there was no correlation between kinetic parameters and tissue nitrogen content. For NO₃^?, both kinetic parameters were higher for plants with low tissue nitrogen than for plants with high tissue nitrogen. Maximum rates were 169 and 75.4 μmol NO₃^?. g dry wt^?1. h^?1, and K_s was 13.3 and 2.31 μM for low and high tissue nitrogen plants, respectively. Estimates of uptake in the field suggested that NH₄⁺ accounted for 65% and NO₃^? for up to 35% of total nitrogen uptake during the summer. Nutrient uptake rates of field-collected plants also indicated that E. prolifera in Yaquina Bay, Oregon was not likely to have been nitrogen-limited, but may have been phosphorus-limited.     

Kinetics of NH4+ and K+ uptake by ectomycorrhizal fungi. Effect of NH4+ on K+ uptake

NH₄⁺ and K⁺ uptake experiments have been conducted with 3 ectomycorrhizal fungi, originating from Douglas fir (Pseudotsuga menziesii (Mirb.] Franco) stands. At concentrations up to 250 μM, uptake of both NH₄⁺ and K⁺ follow Michaelis-Menten kinetics. Laccaria bicolor (Maire) P. D. Orton, Lactarius rufus (Scop.) Fr. and Lactarius hepaticus Plowr. ap. Boud. exhibit K_m values for NH₄⁺ uptake of 6, 35, and 55 μM, respectively, and K_m values for K⁺ uptake of 24, 18, and 96 μM, respectively. Addition of 100 μM NH₄⁺ raises the K_m of K⁺ uptake by L. bicolor to 35 μM, while the V_max remains unchanged. It is argued that the increase of K_m is possibly caused by depolarization of the plasma membrane. It is not due to a competitive inhibition of K⁺ by NH₄⁺ since the apparent inhibitor constant is much higher than the K_m, for NH₄⁺ uptake. The possibility that NH₄⁺ and K⁺ are taken up by the same carrier can be excluded. The K_m, values for K⁺ uptake in the two other fungi are not significantly affected by 100 μM NH₄⁺. Except for a direct effect of NH₄⁺ on influx of K⁺ into the cells, there may also be an indirect effect after prolonged incubation of the cells in the presence of 100 μM NH₄⁺.     

Discrimination of nitrogen isotopes during absorption of ammonium and nitrate at different nitrogen concentrations by rice (Oryza sativa L.) plants

Studies of uptake of ionic sources of N by two hydroponically grown rice (Oryza sativa L.) cultivars (paddy‐field‐adapted Koshihikari and dryland‐adapted Kanto 168) showed that the magnitude of the nitrogen isotope fractionation (?) for uptake of NH₄⁺ depended on the concentrations of NH₄⁺ and cultivar (averaging –6·1‰ for Koshihikari and –12·0‰ for Kanto 168 at concentrations from 40 to 200 mmol m^?3 and, respectively, –13·4 and –28·9‰ for the two cultivars at concentrations from 0·5 to 4 mol m^?3). In contrast, the ? for uptake of NO₃^? in similar experiments was almost insensitive to the N concentration, falling within a much narrower range (+3·2‰ to –0·9‰ for Koshihikari and –0·9‰ to –5·1‰ for Kanto 168 over NO₃^? concentrations from 0·04 to 2 mol m^?3). From longer term experiments in which Norin 8 and its nitrate‐reductase deficient mutant M819 were grown with 2 or 8 mol m^?3 NO₃^? for 30 d, it was concluded that the small concentration‐independent isotopic fractionation during absorption of this ion was not related to nitrate reductase activity.     

Differences in uptake kinetics of ammonium and nitrate in legumes and cereals

Influx isotherms were obtained for nitrate and ammonium from three legumes, Cajanus cajan (L.) Millsp., Cicer arietinum L. and Arachis hypogaea L. and three cereals, Sorghum bicolor (L.) Moench., Pennisetum glaucum L. and Zea mays L. The transition in influx isotherms for both nitrogen sources was found to be within the concentration range (0.05–2.5 mM) tested. There were significant differences in Km and Vmax for ammonium between legumes and cereals. The difference in the kinetic properties for nitrate uptake between the two groups of plants only became apparent at the higher concentration tested. Legumes translocated absorbed nitrate and ammonium to shoots more rapidly than cereals. Results show that there are significant differences in uptake and translocation of ammonium and nitrate between legumes and cereals.     

NUTRITIONAL STUDIES OF TWO RED ALGAE. II. KINETICS OF AMMONIUM AND NITRATE UPTAKE1, 2

Similar NH₄₊ and NO₃^?.uptake kinetic patterns were observed in Neoagardhiella baileyi (Harvey ex Kiitzing) Wyinne & Taylor and Gracilaria foliifera (Forssk?l) Borgesen. NO₃^? was taken up in a rate-sturating fashion described by the Michaelis-Menten equation. NH₄₊ uptake was multicomponent: a saturable component was accompanied by a diffusive or a high K component showing no evidence of saturation (at ≤50 μM [NH₄₊]). Nitrogen starved plantsi(C/N atom ratios > ca. 10) showed higher transient rates of NH₄₊ uptake at a given concentration than plants not N-Iimited. Only plants with high N content exhibited diel changes inNH₄₊ uptake rates, and showed transient rates of NH₄₊ accumulation which did not greatly exceed the capacity to incorporate N in steady-state growth. NH₄₊ was preferred over NO_3?even in plants preconditioned on NO_3?as the sole N. source, NO_3? uptake was suppressed at 5μM [NH₄₊], but simultaneous uptake occurred at unsurpressed rates at lower concentrations. Potential for N accumulation was greater via NH₄₊uptake than via NO_3?uptake. Changing capacity for NH₄₊ uptake with N content appears to be a mechanism whereby excessive accumulation of N was avoided by N-.satiated plants but a large accumulation was possible for N-depleted plants.