Root colonization and iron nutritional status of a Pseudomonas fluorescens in different plant species

Root colonization and induction of an iron stress regulated promoter for siderophore production by Pseudomonas fluorescens 2-79RLI was studied in vitro and in the rhizosphere of different plant species. P. fluorescens 2-79RLI was previously genetically modified with an iron regulated ice nucleation reporter, which allowed calibration of ice nucleation activity with siderophore production. Initial experiments examined ice nucleation activity and siderophore production under different growth conditions in vitro. These studies demonstrated that P. fluorescens 2-79RLI could utilize both Fe-citrate and Fe-phytosiderophore as iron sources, suggesting that production of these compounds by plants would increase iron availability for P. fluorescens 2-79RLI in the rhizosphere. Fe demand and Fe stress were further shown to be a function of nutrient availability and were reduced when carbon was limiting for growth. Subsequent experiments extended these observations to rhizosphere cells. Cells were sampled from the rhizosphere and the rhizoplane. Results of a soil microcosm experiment showed that Fe stress was reduced for P. fluorescens 2-79RLI in the barley rhizosphere as compared to the cells in the rhizosphere.of lupin. In lupin, relative Fe stress of P. fluorescens 2-79RLI was greater at the root tip than in the lateral root zone. In a second experiment comparing zucchini and bean, iron stress was greater for P. fluorescens 2-79RLI associated with zucchini than with bean. In a third experiment with rape plants under P deficient conditions, addition of soluble P was shown to increase Fe stress for P. fluorescens 2-79RLI located at the root tip, but not in the lateral root zone. This study showed that Fe stress of P. fluorescens 2-79RLI in the rhizosphere may be influenced by plant species, P source, root zone and localization of the cells within the rhizosphere.     

Mechanisms of Aluminum Tolerance in Wheat : An Investigation of Genotypic Differences in Rhizosphere pH, K, and H Transport, and Root-Cell Membrane Potentials

Control of rhizosphere pH and exclusion of Al by the plasma membrane have been hypothesized as possible mechanisms for Al tolerance. To test primarily the rhizosphere pH hypothesis, wheat cultivars (Triticum aestivum L. `Atlas 66' and `Scout'), which differ in Al tolerance, were grown in either complete nutrient solution, or 0.6 millimolar CaSO₄, with and without Al at pH 4.50. A microelectrode system was used to simultaneously measure rhizosphere pH, K⁺, and H⁺ fluxes, and membrane potentials (E_m) along the root at various distances from the root apex. In complete nutrient solution, the rhizosphere pH associated with mature root cells (measured 10-40 millimeters from the root apex) of Al-tolerant `Atlas 66' was slightly higher than that of the bulk solution, whereas roots of Al-sensitive `Scout' caused a very small decrease in the rhizosphere pH. In CaSO₄ solution, no significant differences in rhizosphere pH were found between wheat cultivars, while differential Al tolerance was still observed, indicating that the rhizosphere pH associated with mature root tissue is not directly involved in the mechanism(s) of differential Al tolerance. In Al-tolerant `Atlas 66', growth in a CaSO<sub>4</sub> solution with 5 micromolar Al (pH 4.50) had little effect on net K<sup>+</sup> influx, H<sup>+</sup> efflux, and root-cell membrane potential measured in cells of mature root tissue (from 10-40 mm back from apex). However, in Al-sensitive `Scout', Al treatment caused a dramatic inhibition of K⁺ influx and both a moderate reduction of H⁺ efflux and depolarization of the membrane potential. These results demonstrate that increased Al tolerance in wheat is associated with the increased ability of the tolerant plant to maintain normal ion fluxes and membrane potentials across the plasmalemma of root cells in the presence of Al.     

施氮肥和钙肥对烤烟根系形态、生理代谢及产量的影响

为了解氮肥和钙肥对烤烟(Nicotiana tabacum)生长的影响,对成熟期烤烟的根系形态、生理代谢指标和产量进行了研究。结果表明,与施0.12 g kg^-1氮相比,施0.20 g kg^-1氮的烤烟根系最长侧根长、根系体积、根干重、叶干重和可溶性蛋白质含量均极显著升高,MDA含量极显著下降,SOD活性显著下降,但对侧根数、CAT活性和O₂^·的影响均不显著。施钙0.40 g kg^-1,根系体积、侧根数、CAT和SOD活性以及可溶性蛋白质含量均比对照提高,MDA含量和O₂^·则降低;施钙1.00 g kg^-1,最长侧根长、根干重和叶干重均提高。氮×钙互作对烤烟的最长侧根长、根系体积、根干重、叶干重和生理代谢指标的影响均极显著,但对侧根数的影响不显著。因此,施0.20 g kg^-1氮和0.40 g kg^-1钙能最大限度地改善烤烟根系形态、生理状况及提高产量。     

Effect of nitrogen form and phosphorus source on the growth,nutrient uptake and rhizosphere soil property of Camellia sinensis L.

The effects of nitrogen form and phosphorus source on the growth, nutrient uptake and rhizosphere soil property of tea (Camellia sinensis L.) were investigated in a pot experiment. The experiment was performed with a compartmental cropping device, which enables the collection of rhizosphere soil at defined distances from the root of tea plant. Nitrogen was supplied as nitrate or ammonium in combination with soluble phosphorus as Ca(H₂PO₄)₂ or insoluble P as rock phosphate. The leaf dry matter production of tea was significantly greater in the treatments with NH₄ ⁺ than NO₃ ^-, whereas dry matter production of root and stem was not significantly affected. Addition of phosphorus as either source did not influence the dry matter production. The concentrations of K in root, Mg and Ca in both the shoot and root supplied with NO₃ ^- were significantly higher than in NH₄ ⁺ and influence of P sources was minor. On the contrary, Al and Mn concentrations were significantly larger in NH₄ ^--fed plants which could be attributed to remarkably increased availability of Al and Mn caused by acidification of the rhizosphere soil (the first 1-mm soil section from the root surface) with NH₄–N nutrition. The concentration of N in shoot was also significantly higher in NH₄- than in NO₃-fed plants, indicating higher use efficiency of NH₄–N. Whatever the phosphate source, rhizosphere pH declined in ammonium compared to in nitrate treatment. The pH decrease was much larger when no P or soluble P were applied and reached 0.85–1.30 units which extended to 3–5 mm away from the root surface. Exchangeable acidity, content of exchangeable Al and Mn were also considerably higher in the rhizosphere soils of NH₄ ⁺ fed tea plants. Significant amounts of P dissolved from rock phosphate accumulated in rhizosphere of NH₄ ⁺, not NO₃ ^-, suggesting that the dissolution of rock phosphate was induced by the proton excreted by tea root fed with ammonium. With soluble P addition, shoot and root P concentrations were greater in NH₄ ⁺ than in NO₃ ^- treatment and it appeared that this difference could not be sufficiently explained by the available P content in soil which was only slightly higher in NH₄ ⁺ treatment. With rock phosphate addition, the shoot and root P concentrations were hardly affected by nitrogen form, although the available P content was much higher and accumulated in the rhizosphere soil supplied with ammonium. The reason for this was discussed with regard to the inter-relationship of Al with P uptake. This revised version was published online in June 2006 with corrections to the Cover Date.     

Rhizosphere pH along different root zones of Douglas-fir (Pseudotsuga menziesii), as affected by source of nitrogen

Douglas-fir, grown on strongly acid soil (pH-H₂O 3.87), was fertilized with ammonium, nitrate or ammonium nitrate as N-source. Rhizosphere pH along the root axis was measured with microelectrodes. Pure ammonium supply resulted in acidification of the rhizosphere, almost along the entire root axis; only the extreme root tip was slightly alkaline compared with the bulk soil. With nitrate supply, the alkalization of the rhizosphere at the root tip was considerably stronger than with ammonium supply and the length of the alkalization zone greater, extending over the entire growth zone of the root. Acidification of the rhizosphere along the older parts of the root was less pronounced in the case of nitrate. It is concluded that nitrate nutrition enables the plant to protect its most essential root zone from the adverse effects of strong acidity by locally raising the rhizosphere pH.     

Interactions between ammonium and pH of the nutrient solution supplied to gerbera (Gerbera jamesonii) grown in pumice

The interactions between the NH₄-N/total-N supply ratio (N _r) and the pH of the nutrient solution delivered to the plants regarding the nutrient availability and its influence on plant growth and yield were investigated in a gerbera crop grown in pumice. Four treatments obtained by combining a low and a high N _r (0.02 and 0.13 on a molar basis, respectively) with two different levels of nutrient solution pH (5.0 and 5.8, respectively) were compared in a long-term glasshouse experiment. The low N _r resulted in significantly higher pH levels in the rhizosphere, as indicated by the values measured in the drainage water. A high nutrient solution pH further increased pH in the root zone at low N _r but had no influence on it at the higher N _r level. The high pH in the root zone restricted significantly the Cu, Mn, and Zn uptake as indicated by both analytical results and visual symptoms, which were typical for Cu- and Mn-deficiencies. Mn-deficiency was induced only when a low N _r was combined with a high nutrient solution pH. The Cu-deficiency symptoms appeared earlier, were more severe and occurred also when the low N _r was combined with a low nutrient solution pH, but to a lesser extent. As a result of these nutrient deficiencies, both the growth and the flower yield were severely restricted when N _r was low. These results indicate that gerbera is prone to Cu- and Mn deficiencies at pH values above 6 in the rhizosphere. The maintenance of root zone pH below this level in soilless culture is most successfully attained by properly adjusting the NH₄-N/total-N supply ratio rather than the pH of the nutrient solution delivered to the plants.     

Using porewater profiles to assess nutrient availability in seagrass-vegetated carbonate sediments

We measured porewater profiles of inorganic (NH₄ ⁺, NO₃ ^–(+NO₂ ^–), PO₄ ^3– (hereafter referred to as DIP)) and organic (DON, DOP) nutrients in seagrass-vegetated sediments at two sites in a shallow bay in Bermuda within close proximity (200 m) but subject to different nutrient loading. At both sites, total dissolved and inorganic nutrient concentrations were usually 1–2 orders of magnitude higher in the sediments than in the water column, with the exception of NO₃ ^–. Organic N and P were significant components of the total dissolved nutrient pools both in the sediment porewater and in the overlying water column (up to 75% for DON and 40% for DOP), and may be important in meeting plant nutrient demands. We used two approaches to examine how well porewater nutrient concentrations reflected the relative availabilities of N and P for seagrasses: (1) a simple stoichiometric nutrient regeneration model based on the N:P ratio of decomposing organic matter and porewater NH₄ ⁺ concentrations to predict porewater DIP, and (2) fitting of the porewater profiles to estimate rates of net nutrient production (or consumption), which reflects the balance between nutrient sources and sinks in the rhizosphere. The stoichiometric model indicated that sediment porewaters were depleted in P relative to N in the low-nutrient outer bay site, and enriched in P relative to N in the higher-nutrient inner bay site. These results are consistent with the mechanism of carbonate sediments in oligotrophic tropical environments being a strong sink for dissolved inorganic P and our previous work suggesting that nutrient enrichment causes P to become disproportionately more available than N. Net nutrient production rates of porewater P at both sites and N at the inner bay site were low (typically < 2%) relative to the nutrient demands of the seagrasses. The implications of the profile interpretation are two-fold: (1) the low rates of net nutrient production indicate diffusive losses from the root zone were insignificant and that nutrient turnover rates were high, except in the P-limited outer bay where N accumulated in sediment porewaters; and (2) because standing stock nutrient concentrations often represent a small fraction of the total nutrients cycled in the sediments, they are in many cases a poor indicator of nutrient availability. Based on our estimates of losses from the root zone, decomposition, and plant uptake we have constructed a rough budget for the cycling of P and N at our two sites.     

Influence of rhizosphere on the nutrient status of dwarf French beans

French bean seedlings grown on choline, ammoniacal and nitrate forms of nitrogen together with equivalent basal application of P as KH₂PO₄ were tested for nutrient uptake from the rhizosphere. Statistical tests on soil (rhizosphere and non-rhizosphere) and plant (root and shoot) revealed that with the exception of P, levels of all other estimated macro-(Na⁺, K⁺, Ca²⁺, Mg²⁺) and micro-nutrients (Fe²⁺, Mn²⁺, Zn²⁺) were significantly changed after 42 days growth as compared to 21 days growth period. The higher uptake into shoots of Na⁺, K⁺, Fe²⁺, Mn²⁺, Zn²⁺ and H₂PO₄ ⁻ and higher biomass accumulation in the rhizosphere were associated with lower rhizosphere pH. The uptake of Ca²⁺ and Mg²⁺ increased with higher rhizosphere pH. While ammoniacal and choline forms decreased rhizosphere pH and increased the P uptake, nitrate form reversed the trend showing significant inverse relationship between shoot phosphate and rhizosphere pH. Calcium and iron were associated with an inhibition of the translocation of P from root to shoot. However, no causal relationships could be established. Both shoot weight and shoot P content were closely associated with a number of rhizosphere soil parameters. The paper forms a part of the Ph. D thesis submitted by the first author to the University of Wales, 1977.     

External and Internal Root Colonization of Maize by Two Pseudomonas Strains: Enumeration by Enzyme-Linked Immunosorbent Assay (ELISA)

Maize root colonization by two fluorescent Pseudomonas strains M.3.1. and TR335, isolated respectively from maize and tomato roots, were studied in hydroponic conditions. Each bacterium was inoculated separately, and three different colonization areas were studied: nutrient solution, rhizoplane, and endorhizosphere. The two Pseudomonas strains established large rhizosphere populations, and rhizoplane colonization of the entire root system was similar for both strains. However, strain M.3.1. colonized the endorhizosphere more efficiently than strain TR335. Seminal root cuttings from the tip to the seed allowed the assessment of colonization of three different root areas (i.e., root cap and elongation area, root-hair zone, and mature zone). Rhizoplane colonizations of all these three areas by M.3.1. were significantly the same, whereas strain TR335 colonized the rhizoplane of the root cap and elongation area more actively than the root-hair zone and mature zone. Population size of the strain M.3.1. in the internal tissue of these areas was greater than that of strain TR335. Co-inoculations of the two strains indicated a stimulation of the population size of strain M.3.1. regardless of root area studied, whereas population size of strain TR335 remained unchanged. These results demonstrated that external and internal maize root tissues were colonized to a greater extent by a strain isolated from a maize rhizosphere than by one isolated from another rhizosphere. Received: 26 September 1996 / Accepted: 1 November 1996     

Spatial Patterns of Rhizoplane Populations of Pseudomonas fluorescens

Geostatistical analysis was used to compare rhizoplane colonization patterns of an antibiotic-producing biological control bacterium versus a non-antibiotic-producing mutant strain. Pea seeds were inoculated with Pseudomonas fluorescens 2-79RN(inf10) or P. fluorescens 2-79-B46 (a phenazine-deficient Tn5 mutant of P. fluorescens 2-79RN(inf10)) (10(sup8) CFU/pea), planted in sterile sand, and incubated at 20(deg)C. After 3 days, seedlings were prepared for scanning electron microscopy. Photomicrographs (x1,000) of the root surface were taken at the seed-root junction and at 0.5-cm intervals to the root tip. Bacterial counts on the root surface were made in 5- by 5-(mu)m sample units over an area which was 105 by 80 (mu)m. Coordinates and number of bacteria were recorded for each sample unit. Spatial statistics were calculated by covariance for the following directions: omnidirectional, 0, 45, 90, and 135(deg). The ranges of spatial influence and nugget (estimator of spatially dependent variation) were determined. For both P. fluorescens 2-79RN(inf10) and P. fluorescens 2-79-B46, spatial structure was evident along the entire root, particularly in the 0(deg) direction (along the root length) (e.g., range = 24 (mu)m, nugget = 0.52). The degree of spatial dependence observed indicated aggregation of bacterial cells. No differences were detected in the spatial patterns of colonies of P. fluorescens 2-79RN(inf10) and P. fluorescens 2-79-B46, indicating that the lack of phenazine production did not influence spatial patterns on the rhizoplane.     

Proton efflux and transfer cell formation as responses to Fe deficiency of soybean in nutrient solution culture

Hydroponically grown Hawkeye soybeans with N supplied as NO ₃ ^– did not show any measurable pH decrease of the nutrient solution during the first week of Fe deficiency as has been observed for other Fe-efficient dicotyledonous species. Only after prolonged Fe stress with no renewal of the nutrient solution could an unspecific pH reduction be measured as a consequence of a decrease in the NO ₃ ^– content of the solution. On the other hand, Fe stress induced H⁺ efflux could be localized at the root tip region by day foru of-Fe treatment when intact plants were transferred from the nutrient solution to agar medium containing the pH indicator dye bromocresol purple. However, the activity of this H⁺ pump obviously was too weak to neutralize HCO₃-ions simultaneously excreted from older root parts and to acidify the bulk nutrient solution. Thus no remobilization of iron precipitated on older parts of the roots occurred and the plants remained chlorotic.Electron microscopy of the H⁺ extruding zone revealed hypodermal transfer cells with wall protuberances surrounded by cytoplasm especially rich in mitochondria. No transfer cells occurred in the rhizodermis as seen in other Fe-efficient dicots. Some cortical cells also showed transfer cell features with wall protuberances in the intercellular spaces. Often wall ingrowths were surrounded by a periplasmic space which reduced the potential surface amplification of the plasma membrane. It is concluded that the weak capacity of Hawkeye soybeans for Fe stress-induced H⁺ extrusion correlates with their less intense wall labyrinth formation as compared with other dicotyledonous species with higher Fe efficiency.     

Increased Sporulation of Vesicular-Arbuscular Mycorrhizal Fungi by Manipulation of Nutrient Regimens

Adjustment of pot culture nutrient solutions increased root colonization and sporulation of vesicular-arbuscular mycorrhizal (VAM) fungi. Paspalum notatum Flugge and VAM fungi were grown in a sandy soil low in N and available P. Hoagland nutrient solution without P enhanced sporulation in soil and root colonization of Acaulospora longula, Scutellospora heterogama, Gigaspora margarita, and a wide range of other VAM fungi over levels produced by a tap water control or nutrient solutions containing P. However, Glomus intraradices produced significantly more spores in plant roots in the tap water control treatment. The effect of the nutrient solutions was not due solely to N nutrition, because the addition of NH₄NO₃ decreased both colonization and sporulation by G. margarita relative to levels produced by Hoagland solution without P.     

Localization of Nitrate Absorption and Translocation within Morphological Regions of the Corn Root

The absorption of NO₃⁻ was characterized in six regions of a 7-d-old corn root (Zea mays L. cv W64A × W182E) growing in a complete nutrient solution. Based on changing rates of ¹⁵N accumulation during 15-min time courses, translocation of the concurrently absorbed N through each region of the intact root was calculated and distinguished from direct absorption from the medium. Of the ¹⁵N accumulated in the 5-mm root tip after 15 min, less than 15 and 35% had been absorbed directly from the external solution at 0.1 and 10 mm NO₃⁻ concentration of the external solution, respectively. The characterization of the apical portion of the primary root as a sink for concurrently absorbed N was conconfirmed in a pulse-chase experiment that showed an 81% increase of ¹⁵N in the 5-mm root tip during a 12-min chase (subsequent to a 6-min labeling period). The lateral roots alone accounted for 60% of root influx and 70% of 15-min whole root ¹⁵N accumulation at either 0.1 or 10 mm. NO₃⁻ concentration of the external solution. Because relatively steady rates of ¹⁵N accumulation in the shoot were reached after 6 min, the rapidly exchanging pools in lateral roots must have been involved in supplying ¹⁵N to the shoot. The laterals and the basal primary root also showed large decreases (24 and 17%) in ¹⁵N during the chase experiment, confirming their role in rapid translocation.     

Aluminum Resistance in the Arabidopsis Mutant alr-104 Is Caused by an Aluminum-Induced Increase in Rhizosphere pH

A mechanism that confers increased Al resistance in the Arabidopsis thaliana mutant alr-104 was investigated. A modified vibrating microelectrode system was used to measure H⁺ fluxes generated along the surface of small Arabidopsis roots. In the absence of Al, no differences in root H⁺ fluxes between wild type and alr-104 were detected. However, Al exposure induced a 2-fold increase in net H⁺ influx in alr-104 localized to the root tip. The increased flux raised the root surface pH of alr-104 by 0.15 unit. A root growth assay was used to assess the Al resistance of alr-104 and wild type in a strongly pH-buffered nutrient solution. Increasing the nutrient solution pH from 4.4 to 4.5 significantly increased Al resistance in wild type, which is consistent with the idea that the increased net H⁺ influx can account for greater Al resistance in alr-104. Differences in Al resistance between wild type and alr-104 disappeared when roots were grown in pH-buffered medium, suggesting that Al resistance in alr-104 is mediated only by pH changes in the rhizosphere. This mutant provides the first evidence, to our knowledge, for an Al-resistance mechanism based on an Al-induced increase in root surface pH.     

Nutrient composition of Douglas-fir rhizosphere and bulk soil solutions

Rhizosphere soil solution is the direct source of nutrients for plant uptake. The nutrient composition of rhizosphere soil solution can be very different from that of bulk soil solution due to root exudation, nutrient uptake and rhizosphere microorganism activity. This study examined the nutrient composition of Douglas-fir rhizosphere soil solution in two soils belonging to the Nisqually and Pitcher soil series and compared rhizosphere solution with that of bulk soil solution. Fertilized and unfertilized Nisqually soils were also compared. Soil solutions were collected using centrifugation. Results indicated that nutrient concentrations in the rhizosphere solutions were typically higher than that of bulk soil solutions when no fertilizer was applied. Differences in the concentrations of nutrients between the rhizosphere and bulk soil solutions were masked by the addition of fertilizers. Rhizosphere solution pH also appeared to be affected by the concentration of NH₄ and NO₃ in the solution. With a higher concentration of NH₄ relative to NO₃ in the rhizosphere soil solution, the solution pH of the rhizosphere was lower than that of the bulk soil, but with a lower concentration of NH₄ relative to NO₃, the solution pH of the rhizosphere was higher than that of the bulk soil solution.     

FORMATION AND MORPHOLOGY OF AN IRON PLAQUE ON THE ROOTS OF TYPHA LATIFOLIA L. GROWN IN SOLUTION CULTURE

Roots of Typha latifolia L. exposed to Fe²⁺ under reduced conditions in solution culture developed visible coatings (plaques) of an oxidized Fe compound that extended as much as 15-17 μm into the rhizosphere. Iron concentrations were significantly less and discoloration was not apparent on the surface of roots exposed to Fe-(BPDS)₃, Fe³⁺, Fe-EDDHA, and Fe-EDTA. The extent of plaque formation increased with the concentration of Fe²⁺ in solution and with pH of the solution in the range of 3.0 to 4.6. Above pH 4.6, oxidation of Fe²⁺ in the culture solution may have reduced precipitation of Fe on the root surface. Plaque development was most extensive approximately 1.0 cm from the root tip, but all root surfaces showed some Fe staining. Scanning electron micrographs of plaqued roots, grown both in solution culture and in the field, provided support for a model of cast formation by oxidation and precipitation of Fe on external cell surfaces.     

Lateral root formation in pine seedlings

The role of assimilates in lateral root development was studied in Pinus pinea seedlings grown in a nutrient solution. Seedlings were treated with ¹⁴CO₂ for 2 h following removal of the tap root tip at various times prior to the application of ¹⁴CO₂ or removal of a different number of cotyledons at one time. In seedlings with intact root systems most of the radioactivity accumulated in the lower section of the root containing the tap root apex. When the tap root tip was removed, the pattern of radioactivity accumulation along the root was affected by the presence and the stage of lateral root development. Removing the tap root tip of young seedlings (with no lateral roots) resulted in an almost equal distribution of radioactivity along the root. About 50% of the total radioactivity was found in the section showing the highest lateral root growth. Removing the tap root tip of mature seedlings (with lateral roots in the upper section) resulted in an immediate increase in the radioactivity accumulation in the upper section. When lateral roots appeared in the middle section, the pattern of radioactivity distribution was similar to that found in root decapitated young seedlings. Removal of cotyledons of mature seedlings somewhat increased the transport of radioactivity to the lower root section at the expense of the radioactivity in the lateral roots of the upper section. The present study suggests that competition within the root system between the tap root apex and the lateral roots may play an important role in determining the morphology of the root system.     

氮沉降对杉木和枫香土壤氮磷转化及碳矿化的影响

氮沉降是全球变化的重大环境问题,根际是地下生态过程研究的前沿,但目前氮沉降对亚热带地区不同树种土壤氮、磷供应和碳矿化根际过程的影响及其机制尚不清楚。选取典型红壤区15a针叶树杉木(Cunninghamia lanceolata)和阔叶树枫香(Liquidamba formosana)为对象,野外原位开展10 g N m~(-2)a~(-1)氮沉降试验3a,于2014年8月收集杉木和枫香根际土壤和非根际土壤,测定其p H值、有效氮、速效磷、水溶性有机碳及其34 d有机碳矿化动态,并计算根际效应。结果表明:氮沉降显著降低两个树种土壤p H值和杉木根际土壤速效磷(P0.05);提高枫香非根际土壤NO~-_3-N和杉木非根际土壤水溶性有机碳含量。同时,氮沉降显著提高杉木土壤有机碳矿化速率,根际和非根际的增幅分别为71.2%和41.2%,降低枫香土壤有机碳矿化速率,根际和非根际的降幅分别为10.6%和44.1%。此外,氮沉降显著降低枫香土壤NO~-_3-N和有机碳前期矿化速率的根际效应,增强后期矿化速率的根际效应,而杉木对氮沉降响应不显著。可见,氮沉降可显著改变树木土壤养分供应和有机碳稳定性,且丘陵红壤区针叶树和阔叶树根际过程对氮沉降的响应模式有别。率先报道了亚热带不同树种根际碳、氮、磷耦合过程对氮沉降的响应格局,并较好地揭示了针叶树和阔叶树对氮沉降响应的分异机制。     

The chemistry of the lowland rice rhizosphere

Models and experimental studies of the rhizosphere of rice plants growing in anaerobic soil show that two major processes lead to considerable acidification (1–2 pH units) of the rhizosphere over a wide range of root and soil conditions. One is generation of H⁺ in the oxidation of ferrous iron by O₂ released from the roots. The other is release of H⁺ from roots to balance excess intake of cations over anions, N being taken up chiefly as NH₄ ⁺. CO₂ exchange between the roots and soil has a much smaller effect. The zone of root-influence extends a few mm from the root surface. There are substantial differences along the root length and with time. The acidification and oxidation cause increased sorption of NH₄ ⁺ ions on soil solids, thereby impeding the movement of N to absorbing root surfaces. But they also cause solubilization and enhanced uptake of soil phosphate.     

Soil fertility and fine root dynamics in response to 4 years of nutrient (N,P, K) fertilization in a lowland tropical moist forest,Panama

The question of how tropical trees cope with infertile soils has been challenging to address, in part, because fine root dynamics must be studied in situ. We used annual fertilization with nitrogen (N as urea, 12.5 g N m^?2 year^?1), phosphorus (P as superphosphate, 5 g P m^?2 year^?1) and potassium (K as KCl, 5 g K m^?2 year^?1) within 38 ha of old‐growth lowland tropical moist forest in Panama and examined fine root dynamics with minirhizotron images. We expected that added P, above all, would (i) decrease fine root biomass but, (ii) have no impact on fine root turnover. Soil in the study area was moderately acidic (pH = 5.28), had moderate concentrations of exchangeable base cations (13.4 cmol kg^?1), low concentrations of Bray‐extractable phosphate (PO₄ = 2.2 mg kg^?1), and modest concentrations of KCl‐extractable nitrate (NO₃ = 5.0 mg kg^?1) and KCl‐extractable ammonium (NH₄ = 15.5 mg kg^?1). Added N increased concentrations of KCl‐extractable NO₃ and acidified the soil by one pH unit. Added P increased concentrations of Bray‐extractable PO₄ and P in the labile fraction. Concentrations of exchangeable K were elevated in K addition plots but reduced by N additions. Fine root dynamics responded to added K rather than added P. After 2 years, added K decreased fine root biomass from 330 to 275 g m^?2. The turnover coefficient of fine roots <1 mm diameter ranged from 2.6 to 4.4 per year, and the largest values occurred in plots with added K. This study supported the view that biomass and dynamics of fine roots respond to soil nutrient availability in species‐rich, lowland tropical moist forest. However, K rather than P elicited root responses. Fine roots smaller than 1 mm have a short lifetime (<140 days), and control of fine root production by nutrient availability in tropical forests deserves more study.