Potential soil reinforcement by biological denitrification

Currently new ground reinforcement techniques are being developed based on microbially induced carbonate precipitation (MICP). Many studies on MICP use microbially catalyzed hydrolysis of urea to produce carbonate. In the presence of dissolved calcium this process leads to precipitation of calcium carbonate crystals, which form bridges between the sand grains and hence increase strength and stiffness. In addition to urea hydrolysis, there are many other microbial processes which can lead to the precipitation of calcium carbonate. In this study the theoretical feasibility of these alternative MICP processes for ground reinforcement is evaluated. Evaluation factors are substrate solubility, CaCO₃ yield, reaction rate and type and amount of side-product. The most suitable candidate as alternative MICP method for sand consolidation turned out to be microbial denitrification of calcium nitrate, using calcium salts of fatty acids as electron donor and carbon source. This process leads to calcium carbonate precipitation, bacterial growth and production of nitrogen gas and some excess carbon dioxide. The feasibility of MICP by denitrification is tested experimentally in liquid batch culture, on agar plate and in sand column experiments. Results of these experiments are presented and discussed.     

Effects of soil pH and calcium on mycorrhizas of Picea abies

The effects of lime, increased soil pH and increased soil Ca concentration on the mycorrhizas of Norway spruce. [Picea abies (L.) Karst.] were studied independently of each other to elucidate the different mechanisms through which lime may influence mycorrhizas in acidic soil. In a field experiment (mature Norway spruce in podzol), lime was applied as CaCO₃; increased Ca concentration without an increase in pH was achieved with CaSO₄; and soil pH was increased without calcium by means of Na₂CO₃ and K₂CO₃ (Na+K treatment). Treatments were done in October, and mycorrhizas were counted from samples collected in the following June and September. All treatments increased the percentage of dead short root tips compared to controls in September, and Na+K already in June. Cenococcum geophilum Fr. increased in proportion in plots treated with Na+K.In a sand culture experiment, Norway spruce seedlings were grown from seed and inoculated with Cenococcum geophilum, or root inoculum, or left uninoculated. When mycorrhizas were beginning to form, CaCO₃ and CaSO₄ treatments were applied. Six weeks later, the percent of dead short root tips in both salt treatments was significantly increased from control, but formation of mycorrhizas was not inhibited by treatments.As all the treatments increased the proportion of dead short root tips, it is concluded that lime directly and adversely affected mycorrhizas of Norway spruce in sand culture and in mor humus. Both increased ionic strength and increased pH may be reasons for this rather than Ca²⁺ specifically.     

A Novel Approach to Enhance the Urease Activity of Sporosarcina pasteurii and its Application on Microbial-Induced Calcium Carbonate Precipitation for Sand

Abstract

Urease is involved in the formation of carbonate sediments by microbial-induced calcium carbonate precipitation (MICP), and Sporosarcina pasteurii used extensively in this technique owing to its high urease production. In this study, a simple two-step culture method with the appropriate medium was developed to enhance the urease activity of S. pasteurii. Urea played an important role in the culture process, particularly during the pre-cultivation step and the newly developed method improved both urease activity and specific urease activity. Furthermore, the increase in urease activity by MICP resulted in increased production of calcium carbonate and better strength of bio-cemented sand.     

Effect of farm yard manure and CaCO3 on the dry matter yield and nutrient uptake by oats (Avena sativa)

A pot culture experiment was conducted in loamy sand soil to study the effect of different levels of FYM and CaCO₃ on the dry matter yield and nutrients uptake by oats. Application of different levels of CaCO₃ (0, 2, 4 and 8%) and FYM (0, 0.5, 1,2%) resulted in significant increase in dry matter yield of oats. But, a little decrease in dry matter yield was obtained at 4% FYM. The interaction of FYM×CaCO₃ was also significant on dry matter yield of oats. There was a significant decrease in the concentration and uptake of P with increased levels of applied CaCO₃. But, application of FYM resulted in a significant increase in concentration and uptake of P. A significant increase in concentration and uptake of Ca was observed with the increasing levels of CaCO₃. The concentration of Ca decreased with the increased application of FYM in the presence as well as in the absence of added CaCO₃. However, at 0.5 and 1.0 percent FYM with 4 per cent CaCO₃ a little increase in Ca concentration was recorded. The Mg concentration in oat decreased significantly with the increasing levels of CaCO₃ and FYM. The effect of CaCO₃ levels was more pronounced in the absence as well as in the presence of FYM. The Mg uptake followed a different pattern. At 0 and 2% CaCO₃ and application of FYM @ 1 per cent the Mg uptake increased but then it decreased with increasing levels of FYM and CaCO₃ both alone as well as in the presence of each other. The concentration and uptake of Mn decreased with increasing levels of applied CaCO₃. However, in the absence of CaCO₃, the application of FYM increased the concentration and uptake of M_n in oats. In the presence of CaCO₃, Mn concentration decreased at all levels of FYM application but at 8 per cent CaCO₃ there was a slight increase in Mn concentration with 0.5, 2 and 4 percent FYM. Iron concentration and uptake was also affected adversely by increasing levels of CaCO₃ but FYM application removed the harmful effect of CaCO₃ to some extent.     

Characterization of Corn Starch Films Reinforced with CaCO3 Nanoparticles

The characterization of corn starch (CS) films impregnated with CaCO₃ nanoparticles was investigated. Criteria such as morphology, crystallinity, water vapor permeability (WVP), opacity, and mechanical properties were the focus of the investigation. It was found that the CaCO₃ contents had significant effects on the tensile properties of the nanocomposite films. The addition of CaCO₃ nanoparticles to the CS films significantly increased tensile strength from 1.40 to 2.24 MPa, elongation from 79.21 to 118.98%, and Young’s modulus from 1.82 to 2.41 MPa. The incorporation of CaCO₃ nanoparticles increased the opacity of films, lowered the degree of WVP and film solubility value compared to those of the CS films. The results of scanning electron microscopy (SEM) showed that with the increase of CaCO₃ nanoparticles content in starch films, the roughness of the films increased, and pores or cavities were found on the surface of the films, while small cracks were observed in the structures of the fractured surfaces. X-ray diffraction showed that the addition of nanoparticles increased the peaks in the intensity of films.     

A chemical and biological approach towards the definition of calcareous soils

Summary Several agricultural problems are associated with the presence of certain levels of CaCO₃ in soils. The level of CaCO₃ at which the phosphate fixation becomes an apparent agricultural problem, is thought to be an appropriate margine at which the soil can be considered calcareous. Thus, a set of soil mixtures, ranging in CaCO₃ content from 1 to 96% was prepared and used in a column study to determine the level at which the CaCO₃ fraction becomes a dominant factor controlling. P³² movement and distribution.Increasing the percentage of oolitic sand, in the soil mixture, from 1 to 10% caused a sharp drop in P³² movement with soil solution and any increase in CaCO₃ content above 10% did not show any further drop in P³² movement. The amount of P³² removed with the soil solution was generally low compared to that retained in soil columns. Studying the distribution of P³² in soil columns, after five displacements, has indicated that the migration of P³² from the top soil increased by increasing CaCO₃ from 1 and 2 to 6%. The amount of P³² removed was however retained in lower sections. A very sharp decrease in P³² migration from the top soil was observed when CaCO₃ content was raised from 8 to 10%.A similar picture was shown when the CaCO₃ material used was in clay size fraction. However the sharp increase in phosphate retention in top soil sections took place at CaCO₃ content of 8% rather than at 10%. A limit of 8 to 10% CaCO₃ was proposed as an appropriate margine for defining calcareous soils.     

Isolation of alkaliphilic calcifying bacteria and their feasibility for enhanced CaCO3 precipitation in bio-based cementitious composites

Microbially induced calcite precipitation (MICP), secreted through biological metabolic activity, secured an imperative position in remedial measures within the construction industry subsequent to ecological, environmental and economical returns. However, this contemporary recurrent healing system is susceptible to microbial depletion in the highly alkaline cementitious environment. Therefore, researchers are probing for alkali resistant calcifying microbes. In the present study, alkaliphilic microbes were isolated from different soil sources and screened for probable CaCO₃ precipitation. Non-ureolytic pathway (oxidation of organic carbon) was adopted for calcite precipitation to eliminate the production of toxic ammonia. For this purpose, calcium lactate Ca(C₃H₅O₃)₂ and calcium acetate Ca(CH₃COO)₂ were used as CaCO₃ precipitation precursors. The quantification protocol for precipitated CaCO₃ was established to select potent microbial species for implementation in the alkaline cementitious systems as more than 50% of isolates were able to precipitate CaCO₃. Results suggested 80% of potent calcifying strains isolated in this study, portrayed higher calcite precipitation at pH 10 when compared to pH 7. Ten superlative morphologically distinct isolates capable of CaCO₃ production were identified by 16SrRNA sequencing. Sequenced microbes were identified as species of Bacillus, Arthrobacter, Planococcus, Chryseomicrobium and Corynebacterium. Further, microstructure of precipitated CaCO₃ was inspected through scanning electron microscopy (SEM), X-ray diffraction (XRD) and thermal gravimetric (TG) analysis. Then, the selected microbes were investigated in the cementitious mortar to rule out any detrimental effects on mechanical properties. These strains showed maximum of 36% increase in compressive strength and 96% increase in flexural strength. Bacillus, Arthrobacter, Corynebacterium and Planococcus genera have been reported as CaCO₃ producers but isolated strains have not yet been investigated in conjunction with cementitious mortar. Moreover, species of Chryseomicrobium and Glutamicibacter were reported first time as calcifying strains.     

Role of Fungal Mycelium in the Formation of Carbonate Concretions in Growing Media—An Investigation by SEM and Synchrotron-Based X-Ray Tomographic Microscopy

Soil fungi can facilitate calcification. Mushroom Morchella sp . mycelium induced the formation of carbonate concretions on the surface of an organic-based growing media amended with sand and ground limestone. According to SEM observation and X-ray-tomographic microscopy a dense mycelial network induced calcification. The CaCO₃ content of concretions (?: 0.3–1.5 cm) was found to be at 30%. Microsparitic calcite cemented the pores between the sand grains forming a dense clogging microstructure. Besides water uptake by the mycelium, a high evaporation rate and a decrease in pCO₂ contributed to the formation of the concretions. Fungal mycelium in the concretions is surrounded by voids indicating that at the surface of the mycelium, calcification is counteracted most probably by the release of organic acids.     

Effects of different calcium salts on calcium carbonate crystal formation by Sporosarcina pasteurii KCTC 3558

We examined the effectiveness of using different calcium salts for bioconsolidation. Four calcium salts were chosen based on their applicability and solubility. Initial experiments demonstrated that the addition of any calcium salt had a negative effect on the urease activity of S. pasteurii. Microscopic examinations elucidated the morphological and structural differences of the calcium carbonate (CaCO₃) crystals induced. Calcite and vaterite are the prominent forms of CaCO₃ detected according to X-ray diffraction (XRD) analysis. Bioconsolidated sand samples were able to significantly resist water flow through a column compared to the non-treated samples. Also, in a tightness test, the differences in the ability to retain water within columns were observed among the samples tested. Moreover, despite the differences, the calcium salts tested still bound the sand together to form blocks. Our results further explain the influence of multiple factors in crystal formation and sand bioconsolidation effectiveness.     

An Alternative Biotechnological Tool for Magnesite Enrichment: Lactic Acid Bacteria Isolated from Soil

Abstract

Calcium carbonate (CaCO₃) is found in different polymorph structures such as aragonite, vaterite, and calcite. The most common and stable form of CaCO₃, calcite, which is abundant in sedimentary rocks as magnesite ore. Magnesite has application areas in many industrial fields including paper, pharmaceutical and refractory materials. Magnesite is theoretically formulated MgCO₃, but contains many impurities (silicium, iron, and also calcite), that limits its usability and applicability. In this research, we aimed to investigate the decalcification possibility of the raw magnesite material through application of Enterococcus feacelis (EF) with CaCO₃ dissolution ability. The exact mechanism of CaCO₃ dissolution was investigated by carbonic anhydrase enzyme assay and HPLC analysis of organic acids produced by EF. Consequently, EF reduced the amount of CaCO₃ from 2.94% to 0.49% which means a reduction (≈83.33%) in the rate of CaCO₃ percentage. As a result of the experiments, it was observed that different organic acids produced by bacteria reacted with CaCO₃ and removed the lime of magnesite ore. The bacteria used in the study did not show any pathogenic properties in rats, thus, it can be used safely for the industrial applications.     

Bacterial Calcium Carbonate Precipitation in Cave Environments: A Function of Calcium Homeostasis

To determine if microbial species play an active role in the development of calcium carbonate (CaCO ₃ ) deposits (speleothems) in cave environments, we isolated 51 culturable bacteria from a coralloid speleothem and tested their ability to dissolve and precipitate CaCO ₃ . The majority of these isolates could precipitate CaCO ₃ minerals; scanning electron microscopy and X-ray diffractrometry demonstrated that aragonite, calcite and vaterite were produced in this process. Due to the inability of dead cells to precipitate these minerals, this suggested that calcification requires metabolic activity. Given growth of these species on calcium acetate, but the toxicity of Ca ²⁺ ions to bacteria, we created a loss-of-function gene knock-out in the Ca ²⁺ ion efflux protein ChaA. The loss of this protein inhibited growth on media containing calcium, suggesting that the need to remove Ca ²⁺ ions from the cell may drive calcification. With no carbonate in the media used in the calcification studies, we used stable isotope probing with C ¹³ O ₂ to determine whether atmospheric CO ₂ could be the source of these ions. The resultant crystals were significantly enriched in this heavy isotope, suggesting that extracellular CO ₂ does indeed contribute to the mineral structure. The physiological adaptation of removing toxic Ca ²⁺ ions by calcification, while useful in numerous environments, would be particularly beneficial to bacteria in Ca ²⁺ -rich cave environments. Such activity may also create the initial crystal nucleation sites that contribute to the formation of secondary CaCO ₃ deposits within caves.     

Evidences for Bioprecipitation of Pedogenic Calcite by Calcifying Bacteria from Three Different Soils of L'Aquila Basin (Abruzzi,Central Italy)

To provide further evidences on the role of bacterial soil species in the development of calcium carbonate deposits in soil, we isolated 36 heterotrophic bacterial strains from three soils of L'Aquila basin characterized by different CaCO₃ content and tested their ability to precipitate CaCO₃ when cultured on a Ca-rich medium. We found that the majority (63.89%) of these isolates could precipitate CaCO₃ minerals at 27°C. The aptitude to calcification (time and crystal amount) of each calcifying strains, morphology (SEM) and mineralogy of the formed bioliths were also investigated. X-ray diffraction confirmed the production of calcite. Crystal formation was not observed in the controls. Organic matter, total N and assimilable P, cation exchange capacity and exchangeable Ca²⁺, Mg²⁺, K⁺, Na⁺, pH, total and active calcium carbonate content, electric conductivity, skeleton, sand, silt and clay fractions of each soil sample were determined and related with its microbiological parameters. We found that the CaCO₃ content of soil was significatively related, in particular, to the percentage of calcifying bacterial strains (r = 0.95) and to the heterotrophic bacterial density (r = 0.98), which was found significatively related also with Ca²⁺ content of soil (r = ?0.97) and its CEC (r = ?0.97).     

Maltobionic acid enhances intestinal absorption of calcium and magnesium in rats

ABSTRACT

In Experiment 1, the effects of calcium maltobionate (MBCa) on calcium and magnesium absorption were examined using male rats. Four diets were designed in which 25%, 50%, and 100% of calcium carbonate (CaCO₃, Control) were substituted with MBCa and were designated as MBCa-25, MBCa-50, and MBCa-100, respectively. The cecal concentration of short-chain fatty acids was significantly higher in groups MBCa-50 and MBCa-100; however, pH of cecal contents did not significantly differ among the groups. Retention rates of calcium and magnesium were significantly higher in all MBCa groups as compared to the Control. In Experiment 2, the efficiency of calcium absorption was compared using everted sacs of jejunum and ileum with CaCO₃ and MBCa as calcium sources. More calcium from MBCa was absorbed as the concentration of calcium increased in comparison to CaCO₃. It was concluded that MBCa is a better calcium source than CaCO₃ in terms of both calcium retention and absorption.

Abbreviations: ANOVA: analysis of variance; Ca: Calcium; CaCO_3: calcium carbonate; ICP-OES: Inductivity coupled plasma optical emission spectrometer; Mg: magnesium; MBCa: calcium maltobionate; OCPC: o-cresolphthalein complexone; SCFAs: short-chain fatty acids; SE: standard error; TRPM6: transient receptor potential melastatin 6.     

Mull and mor (müller-hesselman) in relation to the soil water regime of a forest

Summary The distribution of mull and mor, in an area which is believed to have borne forest for a number of centuries at least, led to investigations into the reasons for their development.Although the term forest-floor type has been substituted for humus type, mull and mor are used in the Müller-Hesselman sense.There appeared to be no obvious relationship between the distribution of the various forest-floor subtypes and the results of chemical analyses and pH determinations on soil samples.Where free CaCO₃ occurred in the A₁-horizon, a mull forest floor had developed even on coarse sand and the associated herb flora differed only slightly from that occurring on very acid mull. As the manner in which lime influences most soil processes is still unknown, the areas in which free CaCO₃ occurs were excluded from the investigations.Assessments of various other soil characteristics were made and the frequency of association of the various categories of these characteristics ascertained.It is concluded that the colour of the upper part of the A₁-horizon and its degree of leaching are related to its texture, and that the forest-floor subtypes are more closely related to soil texture than to soil colour or degree of leaching.     

Nanoporous CaCO3 Coatings Enabled Uniform Zn Stripping/Plating for Long‐Life Zinc Rechargeable Aqueous Batteries

Zn‐based batteries are safe, low cost, and environmentally friendly, as well as delivering the highest energy density of all aqueous battery systems. However, the application of Zn‐based batteries is being seriously hindered by the uneven electrostripping/electroplating of Zn on the anodes, which always leads to enlarged polarization (capacity fading) or even cell shorting (low cycling stability). How a porous nano‐CaCO₃ coating can guide uniform and position‐selected Zn stripping/plating on the nano‐CaCO₃‐layer/Zn foil interfaces is reported here. This Zn‐deposition‐guiding ability is mainly ascribed to the porous nature of the nano‐CaCO₃‐layer, since similar functionality (even though relatively inferior) is also found in Zn foils coated with porous acetylene black or nano‐SiO₂ layers. Furthermore, the potential application of this strategy is demonstrated in Zn|ZnSO₄+MnSO₄|CNT/MnO₂ rechargeable aqueous batteries. Compared with the ones with bare Zn anodes, the battery with a nano‐CaCO₃‐coated Zn anode delivers a 42.7% higher discharge capacity (177 vs 124 mAh g^?1 at 1 A g^?1) after 1000 cycles.     

A mineralogical characterization of biogenic calcium carbonates precipitated by heterotrophic bacteria isolated from cryophilic polar regions

Precipitation of calcium carbonate (CaCO_3(s)) can be driven by microbial activity. Here, a systematic approach is used to identify the morphological and mineralogical characteristics of CaCO_3(s) precipitated during the heterotrophic growth of micro‐organisms isolated from polar environments. Focus was placed on establishing mineralogical features that are common in bioliths formed during heterotrophic activity, while in parallel identifying features that are specific to bioliths precipitated by certain microbial phylotypes. Twenty microbial isolates that precipitated macroscopic CaCO_3(s) when grown on B4 media supplemented with calcium acetate or calcium citrate were identified. A multimethod approach, including scanning electron microscopy, high‐resolution transmission electron microscopy, and micro‐X‐ray diffraction (μ‐XRD), was used to characterize CaCO_3(s) precipitates. Scanning and transmission electron microscopy showed that complete CaCO_3(s) crystal encrustation of Arthrobacter sp. cells was common, while encrustation of Rhodococcus sp. cells did not occur. Several euhedral and anhedral mineral formations including disphenoid‐like epitaxial plates, rhomboid‐like aggregates with epitaxial rhombs, and spherulite aggregates were observed. While phylotype could not be linked to specific mineral formations, isolates tended to precipitate either euhedral or anhedral minerals, but not both. Three anhydrous CaCO_3(s) polymorphs (calcite, aragonite, and vaterite) were identified by μ‐XRD, and calcite and aragonite were also identified based on TEM lattice‐fringe d value measurements. The presence of certain polymorphs was not indicative of biogenic origin, although several mineralogical features such as crystal‐encrusted bacterial cells, or casts of bacterial cells embedded in mesocrystals are an indication of biogenic origin. In addition, some features such as the formation of vaterite and bacterial entombment appear to be linked to certain phylotypes. Identifying phylotypes consistent with certain mineralogical features is the first step toward discovering a link between these crystal features and the precise underlying molecular biology of the organism precipitating them.     

Availability of Mn as affected by carbonate addition

Summary Addition of CaCO₃ to the soils has been found to increase the retention of manganese applied to soils. As the black soil contained enough of CaCO₃ initially the addition of CaCO₃ even upto 16% is not effective. But in red soil the effect in marked.It has also been observed that addition of CaCO₃, at the rate of 1 to 8 per cent to H-soils, resulted in an increased retention of manganese.The E and r forms decrease and increase respectively with an increase in the addition of CaCO₃ addition to both original and H-soils.Addition of soluble carbonates has also been found to effect the retention of manganese.The availability of manganese added to soils in the soluble form has been found to be adversely affected by the addition of both soluble and in soluble carbonates to black, red, and alkali soils.     

New insights into the role of pH and aeration in the bacterial production of calcium carbonate (CaCO3)

Over recent years, the implementation of microbially produced calcium carbonate (CaCO₃) in different industrial and environmental applications has become an alternative for conventional approaches to induce CaCO₃ precipitation. However, there are many factors affecting the biomineralization of CaCO₃, which may restrict its application. In this study, we investigated the effects of pH and aeration as the main two influential parameters on bacterial precipitation of CaCO₃. The results showed that the aeration had a significant effect on bacterial growth and its rise from 0.5 to 4.5 SLPM could produce 4.2 times higher CaCO₃ precipitation. The increase of pH to 12 resulted in 6.3-fold increase in CaCO₃ precipitation as compared to uncontrolled-pH fermentation. Morphological characterization showed that the pH is an effective parameter on CaCO₃ morphology. Calcite was found to be the predominant precipitate during aeration-controlled fermentations, while vaterite was mainly produced at lower pH (up to 10) over controlled-pH fermentations. Further increase in pH resulted in a morphological transition, and vaterite transformed to calcite at the pH ranges between 10 and 12.

     

Upscaling Effects of Soil Improvement by Microbially Induced Calcite Precipitation by Surface Percolation

This study has contributed to the technology of soil stabilization via biocementation based on microbially induced calcite precipitation. The newly described method of in situ soil stabilization by surface percolation to dry soil under free draining environment is tested for its up-scaling potential. Then, 2-m columns of one-dimensional trials indicated that repeated treatments of fine sand (<0.3 mm) could lead to clogging closed at the injection end, resulting in limited cementation depth of less than 1 m. This clogging problem was not observed in 2 m coarse (>0.5 mm) sand columns, allowing strength varying between 850 to 2067 kPa along the entire 2 m depth. Three-dimensional fine sand cementation trials indicated that relatively homogenous cementation in the horizontal direction could be achieved with 80% of cemented sand cementing to a strength between 2 to 2.5 MPa and to a depth of 20 cm. A simple mathematical model elucidated that the cementation depth was dependent on the infiltration rate of the cementation solution and the in-situ urease activity. The model also correctly predicted that repeated treatments would enhance clogging close to the injection point. Both experimental and simulated results suggested that the surface percolation technology was more applicable for coarse sand.     

Impact of Oxygen Availability on Microbially Induced Calcite Precipitation (MICP) Treatment

Most microbially induced calcite precipitation (MICP) processes are induced by aerobic bacteria; thus, oxygen availability plays an important role in MICP treatment. To determine the effects of oxygen supply on MICP treatment catalyzed by Sporosarcina pasteurii, contrast tests under an aerated condition, air-restricted condition, and open air condition were conducted. The results showed that dissolved oxygen (DO) in the air-restricted reactor decreased with time and was almost exhausted within 7 days; DO in the open box decreased by 50% after 7 days of treatment because of the superficial air supply; and DO in the aerated box maintained an initial high level because the consumed oxygen was supplied immediately by adequate air bubbles in the treatment solution. Unconfined compressive strength (UCS) and CaCO₃ content are high under the aerated condition, moderate under the open condition, and poor under the air-restricted condition. The UCS can be 100 times different depending on the different oxygen supply conditions. The overall influence process is as follows: oxygen is dissolved to supply DO for life and activity of the aerobic urea hydrolysis bacteria; then, urea is hydrolyzed to carbonate anions for CaCO₃ precipitation in the presence of Ca²⁺; and finally, CaCO₃ precipitation results in the strengthening of sand. The results indicate that a sufficient air supply is essential to improve MICP processes catalyzed by aerobic bacteria.