Stem hypertrophic lenticels and secondary aerenchyma enable oxygen transport to roots of soybean in flooded soil

Background and Aims

Aerenchyma provides a low-resistance O₂ transport pathway that enhances plant survival during soil flooding. When in flooded soil, soybean produces aerenchyma and hypertrophic stem lenticels. The aims of this study were to investigate O₂ dynamics in stem aerenchyma and evaluate O₂ supply via stem lenticels to the roots of soybean during soil flooding.

Methods

Oxygen dynamics in aerenchymatous stems were investigated using Clark-type O₂ microelectrodes, and O₂ transport to roots was evaluated using stable-isotope ¹⁸O₂ as a tracer, for plants with shoots in air and roots in flooded sand or soil. Short-term experiments also assessed venting of CO₂ via the stem lenticels.

Key Results

The radial distribution of the O₂ partial pressure (pO₂) was stable at 17 kPa in the stem aerenchyma 15 mm below the water level, but rapidly declined to 8 kPa at 200–300 µm inside the stele. Complete submergence of the hypertrophic lenticels at the stem base, with the remainder of the shoot still in air, resulted in gradual declines in pO₂ in stem aerenchyma from 17·5 to 7·6 kPa at 13 mm below the water level, and from 14·7 to 6·1 kPa at 51 mm below the water level. Subsequently, re-exposure of the lenticels to air caused pO₂ to increase again to 14–17 kPa at both positions within 10 min. After introducing ¹⁸O₂ gas via the stem lenticels, significant ¹⁸O₂ enrichment in water extracted from roots after 3 h was confirmed, suggesting that transported O₂ sustained root respiration. In contrast, slight ¹⁸O₂ enrichment was detected 3 h after treatment of stems that lacked aerenchyma and lenticels. Moreover, aerenchyma accelerated venting of CO₂ from submerged tissues to the atmosphere.

Conclusions

Hypertrophic lenticels on the stem of soybean, just above the water surface, are entry points for O₂, and these connect to aerenchyma and enable O₂ transport into roots in flooded soil. Stems that develop aerenchyma thus serve as a ‘snorkel’ that enables O₂ movement from air to the submerged roots.     

基于树干液流技术的北京市刺槐冠层吸收臭氧特征研究

全球范围内加速的城市化导致空气质量严重退化。随着北京市建设范围不断扩大和机动汽车数量迅猛增长,空气污染日益严重。浓度不断增加的近地层臭氧作为影响全球气候变化的重要因素和危害人类健康、动植物生长的二次污染物,受到广泛关注。城市树木能够有效地去除大气污染物,进而提高空气质量。目前已有很多研究关于区域尺度上城市树木吸收臭氧,然而,冠层尺度上城市树木吸收臭氧特征少有研究。因此,本文基于树干液流技术,结合天气变化和大气臭氧浓度分析,研究夏秋季节北京市典型绿化树种刺槐（Robinia pseudoacacia）整树冠层吸收臭氧特征及环境影响因素。结果表明,在日尺度上,刺槐吸收臭氧速率变化呈单峰曲线,于下午15:00左右达到峰值;夏季峰值范围较宽,秋季峰值范围较窄;中午前后累积吸收臭氧量增加最明显。在季节尺度上,夏季刺槐吸收臭氧速率高于秋季;夏季累积吸收臭氧量显著增加,秋季略有增加。刺槐吸收臭氧的时间变化规律取决于大气臭氧浓度和冠层对臭氧的导度。臭氧浓度日变化和季节变化明显,导致刺槐吸收臭氧速率时间变化格局与之接近。在一定的臭氧浓度下,刺槐吸收臭氧速率的变化主要由冠层对臭氧的导度调控,进而受水汽压亏缺和总辐射的影响。随着水汽压亏缺降低,刺槐冠层对臭氧的导度明显下降;总辐射大于600 W/m2,冠层对臭氧的导度迅速下降。研究树种刺槐单位冠层投影面积上年吸收臭氧量约为0.16 g/m2,明显低于基于模型得到的结果,表明评估森林受臭氧危害的风险应考虑树种冠层臭氧通量。     

Ozone pollution influences soil carbon and nitrogen sequestration and aggregate composition in paddy soils

Background and aims

Much attention has focused on the effects of tropospheric ozone (O₃) on terrestrial ecosystems and plant growth. Since O₃ pollution is currently an issue in China and many parts of the world, understanding the effects of elevated O₃ on soil carbon (C) and nitrogen (N) sequestration is essential for efforts to predict C and N cycles in terrestrial ecosystems under predicted increases in O₃. Thus the main objective of this study was to determine whether an increases in atmospheric O₃ concentration influenced soil organic C (SOC) and N sequestration.

Methods

A free-air O₃ enrichment (O₃-FACE) experiment was started in 2007 and used continuous O₃ exposure from March to November each year during crop growth stage in a rice (Oryza sativa L.)—wheat (Triticum aestivum L.) rotation field in the Jiangsu Province, China. We investigated differences in SOC and N and soil aggregate composition in both elevated and ambient O₃ conditions.

Results

Elevated atmospheric O₃ (18–80 nmol mol^?1 or 50 % above the ambient) decreased the SOC and N concentration in the 0–20 cm soil layer after 5 years. Elevated O₃ significantly decreased the SOC concentration by 17 % and 5.6 % in the 0–3 cm and the 10–20 cm layers, respectively. Elevated O₃ significantly decreased the N concentration by 8.2–27.8 % in three layers at the 20 cm depth. In addition, elevated O₃ influenced the formation and transformation of soil aggregates and the distribution of SOC and N in the aggregates across soil layer classes. Elevated O₃ significantly decreased the macro-sized aggregate fraction (16.8 %) and associated C and N (0.5 g kg^?1 and 0.32 g kg^?1, respectively), and significantly increased the silt+ clay-sized aggregate fraction (61 %) and associated C (1.7 g kg^?1) in the 0–3 cm layer. Elevated O₃ significantly decreased the macro-sized aggregate fraction (9.6 %) and associated C and N (1.4 g kg^?1 and 0.35 g kg^?1, respectively), and significantly increased the silt+ clay-sized aggregate fraction (41.8 %) and decreased the corresponding associated N (0.14 g kg^?1) in the 3–10 cm layer. Elevated O₃ did not significantly effect the formation and transformation of aggregates in the 10–20 cm layer, yet it did significantly increase the C concentration in the macro-sized fraction (1 g kg^?1) and decrease the N concentration in the macro- and micro-sized fractions (0.24 g kg^?1 and 0.16 g kg^?1, respectively).

Conclusion

Long-term exposure to elevated atmospheric O₃ negatively affected the physical structure of the soil and impaired soil C and N sequestration.     

Soil properties and turf growth on a sandy soil amended with fly ash

Field lysimeters of a sandy soil were amended to a depth of 100 mm with four rates (0, 5, 10 and 20%, wt/wt) of fly ash, and effects on soil water content, nutrient leaching, turf growth and nutrition, and uptake of trace elements by turf were assessed. Measurements were taken for 70 days for lysimeters either planted with rhizomes of Cynodon dactylon(L.) Pers., cv. `Wintergreen', or left bare. When irrigated daily, soil water content increased progressively with increasing rates of fly ash and leachate volumes were decreased by 17–52% for lysimeters containing fly ash amended soil. Fertiliser was applied equivalent to 28.4 g N m<sup>–2</sup> and 10.3 g P m<sup>–2</sup> for the entire 70 days (including pre-plant application). Macronutrient concentrations in leaf tissue were within levels regarded as sufficient. Total dry mass (root plus shoot) decreased when fertiliser application rates were reduced by 25%, irrespective of fly ash treatment. In `bare' lysimeters containing fly ash amended soil, cumulative leaching of NO₃ ^–, NH₄ ⁺and P were 0.32–0.88 of the values in non-amended soil. When planted with turf, leaching of those nutrients was minimal (equivalent to 3% of total N applied) and leaching loses did not differ among fly ash rates. Extractable soil P levels were increased 2.5–4.5-fold in the fly ash amended zone, compared with non-amended soil. Root mass in the top 100 mm was 1.2–1.5-fold larger for turf in fly ash amended soil, compared to non-amended soil. The Se concentrations were higher in leaf tissue grown in fly ash amended soil (being at most 0.63 g g^–1), but there was no effect of fly ash amended soil on As, Ba, B, Cd, Co, Cr, Cu, Pb, Hg, Mn, Ni, Ag or Zn in leaf tissues. Thus, fly ash amendment may be a suitable management option for turf culture on sandy soils, since fly ash improved soil water holding capacity and root growth in the amended zone.     

Effect of water deficit on photosynthetic oxygen exchange measured using 18O2 and mass spectrometry in Solanum tuberosum L. leaf discs

The effect of leaf dehydration on photosynthetic O₂ exchange of potato (Solanum tuberosum L., cv. Haig) leaf discs was examined using ¹⁸O₂ as a tracer and mass spectrometry. In normal air (350 μl·l^?1CO₂) and under an irradiance of 390 μmol photons·m^?2·s¹, a relative water deficit (RWD) of about 30% severely decreased net O₂ evolution and increased O₂ uptake by about 50%, thus indicating an enhancement of photorespiration. Increasing CO₂ concentrations diminished O₂ uptake and stimulated net O₂ evolution both in well-hydrated and in dehydrated (RWD of about 30%) leaves. Much higher CO₂ concentrations (up to 4%) were required to observe a complete effect of CO₂ in dehydrated leaves. The chloroplastic CO₂ concentration at the ribulose-1,5-bisphosphate carboxylase-oxygenase (Rubisco) level (C_c) was calculated from O₂-exchange data in both well-hydrated and dehydrated leaves, assuming that the specificity factor of Rubisco was unaffected by desiccation. When plotting net O₂ photosynthesis as a function of C_c, a similar relationship was obtained for well-hydrated and waterstressed leaf discs, thus showing that the main effect of water deficit is a decrease of the chloroplastic CO₂ concentration. At saturating CO₂ levels, the non-cyclic electron-transport rate, measured either as gross O₂ photosynthesis or as the chlorophyll fluorescence ratio (F_m -F_s)/F_m, was insensitive to water deficit, provided RWD was below 40%. In this range of RWD, the decrease in gross O₂ photosynthesis observed in normal air was attributed to the inability of oxidative processes to sustain the maximal electron-flow rate at low chloroplastic CO₂ concentration. The maximal efficiency of photosystem II, estimated as the chlorophyll fluorescence ratio (F_m -F₀)/F_m measured in dark-adapted leaves, was not affected by water deficits up to 60%.     

Distribution of nitrous oxide and regulators of its production across a tropical rainforest catena in the Luquillo Experimental Forest, Puerto Rico

Understanding of N₂O fluxes to the atmosphere is complicated by interactions between chemical and physical controls on both production and movement of the gas. To better understand how N₂O production is controlled in the soil, we measured concentrations of N₂O and of the proximal controllers on its production in soil water and soil air in a field study in the Rio Icacos basin of the Luquillo Experimental Forest, Puerto Rico. A toposequence (ridge, slope-ridge break, slope, slope-riparian break, riparian, and streambank) was used that has been previously characterized for groundwater chemistry and surface N₂O fluxes. The proximal controls on N₂O production include NO₃ ^–, NH₄ ⁺, DOC, and O₂. Nitrous oxide and O₂ were measured in soil air and NO₃ ^–, NH₄ ⁺, and DO were measured in soil water. Nitrate and DOC disappeared from soil solution at the slope-riparian interface, where soil N₂O concentrations increased dramatically. Soil N₂O concentrations continued to increase through the flood plain and the streambank. Nitrous oxide concentrations were highest in soil air probes that had intermediate O₂ concentrations. Changes in N₂O concentrations in groundwater and soil air in different environments along the catena appear to be controlled by O₂ concentrations. In general, N processing in the unsaturated and saturated zones differs within each topographic position apparently due to differences in redox status.     

Influence of Belonolaimus longicaudatus on Nitrate Leaching in Turf

Experiments were conducted to quantify the effects of the sting nematode (Belonolaimus longicaudatus) on root reductions and quantity of nitrate (NO₃ ⁻) leached from ‘Tifdwarf’ bermudagrass in lysimeters. Forty lysimeters were planted with ‘Tifdwarf’ bermudagrass, of which 20 were inoculated with B. longicaudatus and 20 were noninoculated. Root length was compared between treatments at six, 12, and 18 weeks after initiation of the experiments. Turf was fertilized every three weeks, and leaching events were simulated at 21 and 42-day intervals in trial one and trial two, respectively. Leachate was collected, and the quantity of NO₃ ⁻ leached was compared between treatments. Root reductions were observed in lysimeters inoculated with B. longicaudatus at all evaluation dates. Quantity of NO₃ ⁻ leached was greater in inoculated lysimeters at the 18-week evaluation during both trials. This study indicates that nematode damage to turf roots limits root vigor and N uptake, thereby increasing nitrate leaching, adding to water quality concerns.     

Glyceria maxima for wastewater nutrient removal and forage production

Potential biomass yield, nutrient uptake capacity and forage quality of Glyceria maxima was tested in four field lysimeters (I–IV) receiving municipal wastewater. Wastewater was applied during 3 years at different frequencies in order to achieve maximum N-reduction in the system. Accordingly lysimeters III and IV were ponded for part of the week. Harvesting (in June and August) progressively favoured competing terrestrial species in the non-ponded lysimeters (I and II). In year 3 the other species accounted for 65–70% of the harvested biomass in these lysimeters. In the ponded lysimeters (III and IV), reducing conditions in the soil probably prevented terrestrial species from establishing. The total annual yields of the single-species stands in III and IV were 870–1165 gm⁻². Energy, protein, P, K and Ca content of the harvested biomass indicated a high nutritional value. NO₃⁻N concentrations in the harvested biomass varied from 0·08 to 0·32% of dry wt, but did not generally exceed 0·2%.Maximum N and P removed with the harvested biomass was 32 and 4·8 gm⁻² respectively. The relative removal of nutrients in lysimeters III and IV varied from 26 to 55% of the amount of N applied and from 12 to 28% of P applied, which illustrated the possibilities of adjusting the load for optimization of nutrient re-use rather than disposal.     

Responses of the carbon and oxygen isotope compositions of desert plants to spatial variation in soil salinity in Central Asia

We examined the isotopic parameters in two C₃ species (Artemisia diffusa H. Krasch and Tamarix hispida Willd.) and a C₄ species [Haloxylon aphyllum (Minkw.) Iljin.] growing or planted in soils with different levels of salinity in a Central Asian desert. The oxygen isotope ratios of stem water (δ¹⁸O_stem) in T. hispida and H. aphyllum distributed in high-salinity zones were similar to the δ¹⁸O of artesian water (δ¹⁸O_artesian) and different from that in A. diffusa distributed in lower-salinity zones. This indicates that T. hispida and H. aphyllum depend on water with low salinity in the deeper soil layer, whereas A. diffusa depends on water in the shallower soil layer that would be affected by salt accumulation. The carbon isotope composition of leaf organic matter (δ¹³C_om) and oxygen isotope enrichment in leaf organic matter above stem water (Δ¹⁸O_om) were lower in A. diffusa than in the other species. The responses of δ¹³C_om and Δ¹⁸O_om to soil salinity observed for T. hispida suggest that the species decreased its transpiration rate and increased its intrinsic water-use efficiency in response to increasing soil salinity. The δ¹³C_om and Δ¹⁸O_om of H. aphyllum were higher than those of the C₃ species, and were not correlated with soil salinity, suggesting that H. aphyllum reduced its salt uptake by decreasing transpiration—even though it was able to access less saline water in the deeper soil layer. These results indicate that the water-use strategy of desert plants in high-salinity environments can be assessed based on their carbon and oxygen isotope ratios.     

Concentrations of CO2 and O2 in floodwater and in internodal lacunae of floating rice growing at 1–2 metre water depths

Abstract. Environment and plant measurements were made to determine what factors may limit growth of deepwater and floating rice plants during partial or complete submergence. Field surveys included measurements of temperature, pH, light, O₂ and CO₂ in floodwater in Thailand. In addition, measurements were made of O₂ and CO₂ concentrations inside internodal lacunae of deepwater and floating rice growing at 0.5–2.0 m water depths. The bulk of measurements were taken during periods when the changes in water level were less than 50 mm d^?1. In the 0–0.02 m surface layer of floodwater at any location there were large changes in oxygen concentrations over diurnal cycles: there were decreases during the night down to 0.02–0.18 mol m^?3 O₂ at 0600 h and increases during the day to 0.13–0.28 mol m^?3 O₂ at 1500 h (0.28 mol m^?3 being 120% of the O₂ concentration of air saturated water at 30°C). During the day oxygen concentrations decreased with increasing water depth; concentrations just above the soil surface were occasionally zero. Most of this gradient disappeared during the night, and at dawn the 0.6 m surface layer of water had uniform low O₂ concentrations. O₂ concentrations were also measured during flash floods in Thailand. In contrast to the conditions with only small increases in water level, the O₂ concentrations in the water during flash floods were more uniform with depth and changed little over a diurnal cycle, the O₂ ranging between 0.14–0.19 mol m^?3. In most locations floodwater contained 0.2–1.9 mol m^?3 CO₂ and 0.7–1.6 mol m^?3 bicarbonate; however, in a location with acid sulphate soil CO₂ was only 0.05–0.2 mol m^?3, and bicarbonate concentrations were several fold lower. Concentrations of CO₂ in floodwater increased with increasing water depth. O₂ and CO₂ concentrations inside internodal lacunae of rice were determined in the field when water depth were 1–2 m. Concentrations of O₂ in internodes at the water surface were 16–20%, and decreased to 10% and 5% at 0.8 and 1.8 m water depth respectively. There was no diurnal cycle in O₂ concentrations inside internodes. In contrast, CO₂ concentrations in the lacunae increased with water depth and ranged from 1–3% in internodes at the water surface to 5–10% in internodes at 1.8 m water depth. There was evidence for a diurnal cycle in CO₂ concentrations in the basal internode near the soil surface, CO₂ increased during the day and decreased during the night. The above data are used to show that there is little or no relationship between gas concentrations in floodwater and internodal lacunae of rice plants. Results are discussed in relation to O₂ supply to submerged portions of rice and metabolism of these tissues at low O₂ concentrations.     

Postillumination respiration of maize in relation to oxygen concentration and glycolic Acid metabolism

Prior illumination in CO₂-free air enhances a respiration from maize (Zea mays L.) leaves different in onset and duration from the postillumination burst of photorespiration. The course of respiration after brief illumination of attached leaves was measured as CO₂ efflux in darkness into CO₂-free atmospheres with four O₂ concentrations. The peak of CO₂ efflux following illumination was suppressed by 2.23% O₂, was completely eliminated by 0.04% O₂, and was not stimulated by 40% O₂ compared with air. Compared with air, steady dark respiration was suppressed by 0.04% O₂ but was not affected by 2.23% nor 40% O₂. Excision and subsequent uptake of distilled water through the vascular system nearly eliminated the enhanced respiration.     

Effects of soil warming and nitrogen fertilization on leaf physiology of Pinus tabulaeformis seedlings

The paper mainly studied the short-term influences of experimental warming, nitrogen addition, and their combination on physiological performance of P. tabulaeformis seedlings. Free air temperature increase system of infrared heaters was used to raise monthly average soil and air temperature by 2.6 and 2.1?°C above the ambient. NH₄NO₃ solution was added for a total equivalent to 25?g?N?m^?2?a^?1. Experimental warming and nitrogen addition induced a significant increase in leaf nitrogen concentration, A _max, ??, antioxidant enzymes activities, ASA and free proline contents, but both of them sharply decreased AOS and MDA level. Interestingly, the interaction of warming and nitrogen fertilization further improved leaf nitrogen concentration, A _max, ??, and antioxidant compounds accumulation, and also resulted in lower rate of O₂ ^? production than either single warming or fertilization. Obviously, the beneficial effects of warming and N fertilization alone on leaf physiology of P. tabulaeformis seedlings were magnified by the combination.     

Estimation of Nitrification and Denitrification from Microprofiles of Oxygen and Nitrate in Model Sediment Systems

The coupling between nitrification and denitrification and the regulation of these processes by oxygen were studied in freshwater sediment microcosms with O₂ and NO₃^- microsensors. Depth profiles of nitrification (indicated as NO₃^- production), denitrification (indicated as NO₃^- consumption), and O₂ consumption activities within the sediment were calculated from the measured concentration profiles. From the concentration profiles, it was furthermore possible to distinguish between the rate of denitrification based on the diffusional supply of NO₃^- from the overlying water and the rate based on NO₃^- supplied by benthic nitrification (D_w and D_n, respectively). An increase in O₂ concentration caused a deeper O₂ penetration while a decrease in D_w and an increase in D_n were observed. The relative importance for total denitrification of NO₃^- produced by nitrification thus increased compared with NO₃^- supplied from the water phase. The decrease in D_w at high oxygen was due to an increase in diffusion path for NO₃^- from the overlying water to the denitrifying layers in the anoxic sediment. At high O₂ concentrations, nitrifying activity was restricted to the lower part of the oxic zone where there was a continuous diffusional supply of NH₄⁺ from deeper mineralization processes, and the long diffusion path from the nitrification zone to the overlying water compared with the path to the denitrifying layers led to a stimulation in D_n.     

Flux-based ozone risk assessment for adult beech forests

Tropospheric ozone (O₃) is a critical threat to forest ecosystems. A stomatal flux-based risk evaluation methodology at the leaf level was established recently in the context of the Convention on Long-Range Transboundary Air Pollution (LRTAP). This study demonstrates improvement and validation of the stomatal flux-effect approach for adult beech with results from the 8-year free-air O₃ enrichment experiment at “Kranzberger Forst” (Germany). The risk assessment module of the SVAT model FO₃REST, being under development for local scale O₃-risk assessment of adult beech stands, was parameterized according to the LRTAP Convention’s Mapping Manual. Mean maximum stomatal conductance for water vapour of 245?mmol H₂O m^?2 PLA s^?1, as suggested in the LRTAP Convention’s Mapping Manual for beech, was affirmed by assessment at “Kranzberger Forst”, resulting in 162?mmol O₃ m^?2 PLA s^?1 upon recommended adjustment of the O₃/water vapour diffusivity ratio to 0.663. Based on this ratio, a provisional corrected flux-effect function was deduced. Modelled Phytotoxic O₃ Doses (POD ₁) and potential O₃-caused losses in biomass formation estimated with a site-specific stomatal conductance algorithm differed slightly only from estimates by the original LRTAP parameterisation. Analysis-derived POD ₁ target value within the meaning of Article 2 of the European Council Directive 2008/50/EC of 10?mmol O₃ m^?2 corresponded to potential loss in biomass formation of about 10?% in ambient air relative to “pre-industrial” conditions. However, exceedance occurred by about a factor of two during the study period, indicating high risk at “Kranzberger Forst” under ambient air. Assessment for doubled O₃ exposure indicated potential underestimation even of the O₃ risk because modelled losses in biomass formation are in the lower range of the standard deviation of the observed ones.     

Field evaluation on functional roles of root plastic responses on dry matter production and grain yield of rice under cycles of transient soil moisture stresses using chromosome segment substitution lines

Background and Aims

The tall fern (Athyrium distentifolium Tausch ex Opiz) forms large stands in many deforested sites in Central European mountains. In the present study, we want to demonstrate that the effect of ferns on the leaching of nutrients is the same at low and high nitrogen (N) deposition.

Methods

Free-tension lysimeters with growing ferns, and some with bare forest soil were installed in field conditions in 2006. We monitored the chemistry of lysimetric water at ambient and enhanced (plus 50?kg?N ha^-1) levels of N deposition during five growing seasons.

Results

Results indicate that during the growing seasons ferns slightly decreased of acidity and conductivity of lysimetric water and substantially reduced losses of base cations (Ca²⁺ and Mg²⁺). The concentration of leached base cations was three to seven times higher from bare forest soil than from lysimeters with ferns. Higher N accumulation in fern biomass coincides with lower contents of leached N in lysimetric water.

Conclusions

The reduced losses of base cations were due to the ability of Athyrium to absorb and accumulate nutrients in large amounts in living biomass and in dead undecomposed plant matter and particularly in below-ground biomass.     

Simulation Model of the Coupling between Nitrification and Denitrification in a Freshwater Sediment

A model was constructed to simulate the results of experiments which investigated nitrification and denitrification in the freshwater sediment of Lake Vilhelmsborg, Denmark (K. Jensen, N. P. Sloth, N. Risgaard-Petersen, S. Rysgaard, and N. P. Revsbech, Appl. Environ. Microbiol. 60:2094-2100, 1994). The model output faithfully represented the profiles of O₂ and NO₃^- and rates of nitrification, denitrification, and O₂ consumption as the O₂ concentration in the overlying water was increased from 10 to 600 μM. The model also accurately predicted the response, to increasing O₂ concentrations, of the integrated (micromoles per square meter per hour) rates of nitrification and denitrification. The simulated rates of denitrification of NO₃^- diffusing from the overlying water (D_w) and of NO₃^- generated by nitrification within the sediment (D_n) corresponded to the experimental rates as the O₂ concentration in the overlying water was altered. The predicted D_w and D_n rates, as NO₃^- concentration in the overlying water was changed, closely resembled those determined experimentally. The model was composed of 41 layers 0.1 mm thick, of which 3 represented the diffusive boundary layer in the water. Large first-order rate constants for nitrification and denitrification were required to completely oxidize all NH₄⁺ diffusing from the lower sediment layers and to remove much of the NO₃^- produced. In addition to the flux of NH₄⁺ from below, the model required a flux of an electron donor, possibly methane. Close coupling between nitrification and denitrification, achieved by allowing denitrification to tolerate some O₂ (~10 μM), was necessary to reproduce the real data. Spatial separation of the two processes (no toleration by denitrification of O₂) resulted in too high NO₃^- concentrations and too low rates of denitrification.     

Effects of air-filled soil porosity and aeration on the initiation and growth of secondary roots of maize (Zea mays)

We studied the possibility whether the initiation of secondary roots is regulated by the air-filled porosity in soil, i.e. the availability of oxygen in the soil. Maize plants were grown in long PVC tubes (1 m long and 12 cm diameter) and were unwatered for different numbers of days so that variations of soil water content with depth were achieved on the same date with plants at the same age. The plants were harvested when their root systems were established in the whole soil column and watering had been withheld for 0, 15, 20, 25 days. A decrease of soil water content was significantly correlated with an increase of air-filled porosity in soil. The number of secondary lateral roots from segments of primary adventitious roots increased dramatically when soil water content decreased from field capacity to about 0.05 g water g^-1 dried soil. The total dried mass of roots at different soil depths was also positively correlated with soil air-filled porosity. It was observed that the elongation of the initiated secondary roots responded differently to the variations of soil air-filled porosity. The length of secondary roots increased initially when the soil was dried from field capacity to 0.18 g g^-1 dried soil (water potential at about−0.2 MPa, air-filled porosity 0.26 cm³ cm^-3), but was drastically reduced when the soil was dried further. Obviously elongation of secondary roots was inhibited when soil water potential began to deviate substantially from an optimum value. The present results suggested that the initiation of secondary roots was greatly promoted by the increase of air-filled soil porosity, i.e. availability of oxygen. This conclusion was further verified in a separate experiment where solution-cultured maize seedlings were subjected to different aeration treatments. An obvious increase in secondary root initiation was found in plants which were aerated with normal air (21% O₂) than in plants which were either not aerated or aerated with 5% O₂ air. ei]Section editor: B E Clothier     

Flow velocity affects internal oxygen conditions in the seagrass Cymodocea nodosa

The internal oxygen status of seagrass tissues, which is believed to play an important role in events of seagrass die-off, is partly determined by the rates of gas exchange between leaves and water column. In this study, we examined whether water column flow velocity has an effect on gas exchange, and hence on internal oxygen partial pressures (pO₂) in the Mediterranean seagrass, Cymodocea nodosa. We measured the internal pO₂ in the horizontal rhizomes of C. nodosa in darkness at different mainstream flow velocities, combined with different levels of water column oxygen pO₂ using an experimental flume in the laboratory. Flow velocity clearly had an effect on the internal oxygen status. In stagnant, but fully aerated water the mean internal pO₂ was 6.9 kPa, corresponding to about 30% of air saturation. The internal pO₂ increased with increasing flow velocity reaching saturation of around 12.2 kPa (60% of air saturation) at flow velocities ≥7 cm s⁻¹. Flow had a relatively larger influence on internal pO₂ at lower water column oxygen concentrations. By extrapolating linear relationships between internal and water column pO₂ in this experimental setup, rhizomes would become anoxic at a water column oxygen pO₂ of 4–4.5 kPa (∼20% of air saturation) in flowing water, but already at 6.4 kPa (∼30% of air saturation) in stagnant water. Water flow may play an important role for seagrass performance and survival in areas with poor water column oxygen conditions and may, in general, be of importance for the distribution of submerged rooted plants.     

Aerial and Aquatic Respiration in the River Crab Potamonautes Warreni Calman with Notes on Gill Structure

Summary

The oxygen consumption rate (?O₂) for Potamonauteus warreni Calman (= Potamon warreni (Calman) kept in 25 °C water was 34,4 μmol 1^?1 O₂ kg^?1 and after 72 hours in 98% R.H. air the rate was 31,9 μmol 1^?1 O₂ kg^?1 min^?1. The ?O₂ values for each of the two groups are not significantly different (P > 0,05). The partial oxygen tension of pre-branchial (v = venous) haemolymph (P_vCO₂) is 15,3 mm Hg in water and 13,0 mm Hg in air); partial carbon dioxide tension of pre-branchial (v) haemolymph (P_vCO₂) is 13,2 mm Hg in water and 13,0 mm Hg in air); the total carbon dioxide concentration in pre-branchial (v) haemolymph (C_vCO₂) tot. is 12,3 mmol 1^?1 in air and 13,9 mmol 1^?1 in water) are not significantly different for the two groups (P > 0,05). The haemolymph pH and the lactate concentration for crabs in water was found to be 7,51 and 0,38 mmol 1^?1 respectively. No significant differences were found in pre-branchial haemolymph oxygen tension, carbon dioxide tension, total carbon dioxide content, haemolymph pH, lactate level, chloride concentration, P₅₀ and haemocyanin-oxygen cooperativity in control crabs kept in water, and experimental crabs held in air for 72 hours. The chloride concentration, (327,0 mmol 1^?1) for crabs kept in water does not differ from that of crabs held in air for 72 hours but is at least 15% higher than the sodium concentration (255 mmol 1^?1) for crabs kept in water. The gill surface area is 520 mm² g^?1 wet body mass; on average 9,2 gill platelets (lamellae) can be found on a gill length of one millimetre. Each lamella is spaced 60–70 μm apart, each with a thickness of 30–40 μm. It is concluded that P. warreni may be described as a truly amphibious fresh-water crab.     

The Regulation of Photosynthesis in Leaves of Field-Grown Spring Wheat (Triticum aestivum L., cv Albis) at Different Levels of Ozone in Ambient Air

Wheat (Triticum aestivum L. cv Albis) was grown in open-top chambers in the field and fumigated daily with charcoal-filtered air (0.015 microliters per liter O₃), nonfiltered air (0.03 microliters per liter O₃), and air enriched with either 0.07 or 0.10 microliters per liter ozone (seasonal 8 hour/day [9 am-5 pm] mean ozone concentration from June 1 until July 10, 1987). Photosynthetic ¹⁴CO₂ uptake was measured in situ. Net photosynthesis, dark respiration, and CO₂ compensation concentration at 2 and 21% O₂ were measured in the laboratory. Leaf segments were freeze-clamped in situ for the determination of the steady state levels of ribulose 1,5-bisphosphate, 3-phosphoglycerate, triose-phosphate, ATP, ADP, AMP, and activity of ribulose, 1,5-bisphosphate carboxylase/oxygenase. Photosynthesis of flag leaves was highest in filtered air and decreased in response to increasing mean ozone concentration. CO₂ compensation concentration and the ratio of dark respiration to net photosynthesis increased with ozone concentration. The decrease in photosynthesis was associated with a decrease in chlorophyll, soluble protein, ribulose bisphosphate carboxylase/oxygenase activity, ribulose bisphosphate, and adenylates. No decrease was found for triose-phosphate and 3-phosphoglycerate. The ratio of ATP to ADP and of triosephosphate to 3-phosphoglycerate were increased suggesting that photosynthesis was limited by pentose phosphate reductive cycle activity. No limitation occurred due to decreased access of CO₂ to photosynthetic cells since the decrease in stomatal conductance with increasing ozone concentration did not account for the decrease in photosynthesis. Ozonestressed leaves showed an increased degree of activation of ribulose bisphosphate carboxylase/oxygenase and a decreased ratio of ribulose bisphosphate to initial activity of ribulose bisphosphate carboxylase/oxygenase. Nevertheless, it is suggested that photosynthesis in ozone stressed leaves is limited by ribulose bisphosphate carboxylation possibly due to an effect of ozone on the catalysis by ribulose bisphosphate carboxylase/oxygenase.