Influence of storage on soil microbial biomass estimated by three biochemical procedures

The effects of 28 and 56 days' storage at 25°, 4° and ?20°C on the microbial biomass content of four soils from tussock grasslands were studied by three biochemical procedures. Two of the procedures involved measurement of CO₂ and mineral-N (Min-N) production by chloroform-fumigated and unfumigated soil, and consequent estimation of biomass C and Min-N flush respectively. In the third, adenosine 5'-triphosphate (ATP) content was determined.Patterns of CO₂ production were often influenced by storage treatment. The use of fixed incubation periods for estimating the CO₂ flush of fumigated soil and the steady rate of CO₂ production by unfumigated soil did, however, give biomass C estimates that were generally similar to those calculated from individually determined incubation periods for each treatment and soil.Biomass C values could change significantly at all storage temperatures, but generally least at ?20°C. Storage at ?20°C was also the most suitable for retaining ATP contents, whereas 4°C was best for values of Min-N flush. Values of Min-N flush after storage of soil at ?20°C decreased significantly in two of the soils but increased in another. No storage temperature was thus satisfactory for all three indices of microbial biomass. Generally, however, 4°C was adequate for short periods, and 25°C the least suitable.     

A simple method for quantitative determination of ATP in soil

A simple method to measure soil ATP by the luciferin-luciferase system is described. The ATP is extracted from the soil by vigorous shaking with a sulfuric acid-phosphate solution for 15 min. An aliquot of the soil suspension is neutralized with a Tris-EDTA solution and mixed with a special ATP releasing reagent (NRB). ATP is measured after a 10 s exposure to the NRB reagent, followed by addition of luciferin-luciferase and integration over 10 s in a Lumacounter M 2080. The ATP content in soils which had been stored at 5°C for 90 days and then incubated at 25°C for 5 days, ranged from 0.37 to 7.52 μg ATP g^?1 dry wt, with standard deviations less than 10%. There was a close (r = 0.96) linear relationship between ATP content and biomass C determinated by fumigation for this group of soils. The soil biomass contained 4.2–7.1 μg ATP mg^?1 biomass C. The ATP content of the biomass declined during storage at 5°C for 210 days.     

Fluctuations in microbial biomass indices at different sampling times in soils from tussock grasslands

Microbial biomass in four topsoils from New Zealand tussock grasslands was estimated by three biochemical procedures at five sampling times over a 15 month period. In Conroy, Cluden and Tima soils, biomass C content was high in two sets of March (summer-autumn) samples and low in October (early spring) samples; in Carrick soil from a wetter, cooler environment, it was similar at all sampling times. Significant time-of-sampling variations occurred with Min-N flush in Tima and Carrick soils, and with adenosine 5'-triphosphate (ATP) content in three of the soils. Generally, the ratios of these biomass indices also varied significantly at some sampling times. Because of this variability, common factors could not validly be used with these soils for estimating biomass C contents from Min-flush or ATP values.The contribution of bacteria and fungi to the respiratory activity of the microbial biomass was unsuccessfully investigated using streptomycin and actidione as differential inhibitors of anabolic metabolism in the presence of added glucose. In three of the soils, rates of O₂ uptake did not generally increase significantly during incubation, even with added N, P, K and S or prior incubation overnight. In Conroy soil, rates did increase significantly, but the effects of the antibiotics separately and together could not be satisfactorily balanced.     

Adenosine triphosphate and microbial biomass in soil

Two methods for measuring adenosine 5'-triphosphate (ATP) in soil were compared, one based on extraction with NaHCO₃-CHCl₃ and thel other on extraction by a trichloracetic acid-phosphate-paraquat reagent. Recoveries of added ATP were greater with the NaHCO₃-CHCl₃ reagent but the extraction of “native” soil ATP by NaHCO₃-CHCl₃ was only about a third of that by TCA-phosphate-paraquat.Microbial biomass C and ATP were measured in 8 contrasting English soils, using the fumigation method to measure biomass C and the TCA-phosphate-paraquat method to measure ATP. Except in one acid woodland soil, the ratio (ATP content of the soil)/(biomass C content of the soil) was relatively constant, with a mean of 7.3 mg ATP g^?1 biomass C for the different soils. This value is very similar to that obtained earlier in a range of 11 grassland and arable soils from Australia. Taking the English and Australian grassland and arable soils together, there is a close (r = 0.975) linear relationship between ATP and microbial biomass C that holds over a wide range of soils and climates. From this relationship, the soil biomass contains 7.25 mg ATP g^?1 biomass C, equivalent to an ATP-to-C ratio of 138, or to 6.04 μmoles ATP g^?1 dry biomass.The acid woodland soil (pH 3.9) contained much less biomass C, as measured by the fumigation method, than would have been expected from this relationship. This, and other evidence, suggests that the fumigation method for measuring microbial biomass C breaks down in strongly acid soils.The ATP content of the biomass did not depend on the P status of the soil, as indicated by NaHCO₃-extractable P.     

Microbial biomass in soil: Effects of some experimental variables on biochemical estimations

The effects of experimental variables on estimates of biomass C and mineral-N (Min-N) flush by the chloroform fumigation technique were determined in near neutral to slightly alkaline topsoil samples of a Typic Haplaquoll taken at three different times under grazed grass-clover pastures. The variables were soil mesh size ( < 3.3 and < 2 mm), water content [50 and 60% of water-holding capacity (WHC)], the use of samples that were “fresh” or that had been previously incubated (7 days at 50% of WHC at 25°C), and, for the biomass C estimates, various incubation periods for measuring CO₂C production.Estimates of biomass C were most strongly influenced by the incubation period selected for CO₂C production by unfumigated soil. The effects of soil mesh size and water content were significant for some samples, but were not consistent. Prior incubation lowered all biomass C estimates significantly, except for some samples where a 0–10 day period was used for measuring CO₂C production by unfumigated soil; (the presence or absence of soda-lime during incubation had no influence on subsequent rates of CO₂ production by the unfumigated samples).Min-N flush was not consistently influenced by these variables, although some significant treatment effects occurred. Biomass C-to-Min-N flush ratios were predictably dependent upon the biomass C estimates used. They averaged 9.0 in “fresh” samples and 6.0 in incubated samples, when the incubation periods for CO₂C production by unfumigated samples were 10–20 and 0–10 days respectively.Results indicate that care should be taken in interpreting and comparing biochemical indices of microbial biomass, and their ratios, obtained by different or modified experimental procedures.     

Microbial biomass and activity in an agricultural soil with different organic matter contents

Changes in soil fertility caused by various organic and N-fertilizer amendments were studied in a long-term field trial mostly cropped with cereals. Five treatments were included: (I) fallow, (II) cropping with no C or N addition, (III) cropping with N-fertilization (80 kg ha ^?1 yr^?1), (IV) cropping with straw incorporation (1800kg Cha^?1 yr^?1) and N-fertilization (80 kg ha^?1yr^?1), and (V) cropping with addition of farmyard manure (80 kg N + 1800kg Cha^?1yr^?1). The treatments resulted in soil organic matter contents ranging from 4.3% (I) to 5.8% (V). Microbial biomass and activity were determined by chloroform fumigation, direct counting of fungi (fluorescein diacetate (FDA)-staining and Jones-Mollison agar-film technique) and bacteria (acridine orange staining), most probable number determinations of protozoa, esterase activity (total FDA hydrolysis) and respiration. Both biomass estimates and activity measurements showed a highly significant correlation with soil organic matter. Microbial biomass C ranged from 230 to 600 μg C g^?1 dry wt soil, as determined by the fumigation technique, while conversions from direct counts gave a range from 380 to 2260 μg C. Mean hyphal diameters and mean bacterial cell volumes decreased with decreasing soil organic matter content.     

Adenosine triphosphate (ATP) and microbial biomass in soil: Effects of storage at different temperatures and at different moisture levels

Abstract

On air‐drying, the ATP contents of two moist soils fell to about one quarter of their original values. When a freshly‐sampled soil (field temperature 5.5°C) was stored moist (43% water holding capacity) for 7 days at 25°C the ATP content increased from 4.54 to 7.84 μg ATP g^‐1 soil. Storage at 10°C caused a smaller increase; to 5.39 μg g^‐1 soil. Microbial biomass C also increased on storage but the relative increase was less than that of ATP. Thus the biomass C/ATP ratio fell from 234 in the freshly sampled soil to 168 in the soil stored moist for 7 days at 25°C. The ATP content declined to less than half its starting value if storage was under waterlogged conditions.

The ATP method for determining microbial biomass in soil depends on the use of a constant factor (5.85 mg ATP g^‐1 biomass C) for converting ATP content to biomass C. This factor came from work on soils that had been stored moist at 25°C for several days before biomass C and ATP measurements were made: it is only applicable to soils that have been stored in this way.     

Phosphorus in the soil microbial biomass

Phosphorus in the soil microbial biomass (biomass P) and soil biomass carbon (biomass C) were linearly related in 15 soils (8 grassland, 6 arable, 1 deciduous woodland), with a mean P concentration of 3.3% in the soil biomass. The regression accounted for 82% of the variance in the data. The relationship was less close than that previously measured between soil biomass C and soil ATP content and indicates that biomass P measurements can only provide a rough estimate of biomass C content. Neither P concentration in the soil biomass, nor the amount of biomass P in soil, were correlated with soil NaHCO₃-extractable inorganic, organic or total P.The calculated mean annual flux of P through the biomass (in a soil depth of 10 cm) in 8 grassland soils was large, 23 kg P ha^?1 yr^?1, and more than three times the mean annual P flux through 6 arable soils (7 kg P ha^?1 yr^?1), suggesting that biomass P could make a significant contribution to plant P nutrition in grassland.About 3% of the total soil organic P in the arable soils was in microbial biomass and from 5 to 24% in the grassland soils. The decline in biomass P when an old grassland soil was put into an arable rotation for about 20 yr was sufficient to account for about 50% of the decline in total soil organic P during this period. When an old arable soil reverted to woodland, soil organic P doubled in 100 yr; biomass P increased 11-fold during the same period.     

A method for measuring adenosine triphosphate in soil

A method was devised for the extraction and measurement of adenosine 5'-triphosphate (ATP) in soil that minimizes sorption of ATP on the soil colloids. Soil was ultrasonified for 1 min with a solution containing trichloracetic acid (0.5 m). disodium hydrogen orthophosphate (0.25 m) and paraquat dichloride (0.1 m). The ATP content of the filtered extract was determined without further treatment in a scintillation spectrometer by the firefly luciferin-luciferase system. Recovery of added ATP was greater using the extratant containing trichloracetic acid, orthophosphate and paraquat than with trichloracetic acid alone or with a sulphuric acid extradant. Recoveries of added ATP ranged from 45% to 84% in thirteen different soils; ATP contents from 0.64 to 9.03 μg g^?1 soil.     

Microbiological and biochemical characteristics of a range of New Zealand soils under established pasture

Twenty one topsoils, selected to represent major New Zealand soil groups were collected from developed, grazed pasture and examined for microbiological and biochemical characteristics. Organic C and total N levels ranged from 2.4–46% (mean 8.7%) and 0.22–2.31% (mean 0.65%), respectively. The characteristics examined included microbial biomass (mean 1240 μg Cg^?1 soil), min-N flush (mean 85 μg N g^?1 soil), microbial P (mean 52 μg P g^?1 soil), min-N and CO₂ produced, nitrification index, urease, protease, phosphatase and arylsulphatase activities. Most of these characteristics were generally higher than the values already published possibly due to high levels of organic matter.Principal component analysis of the correlation matrix showed two distinct groups of characteristics: CO₂ produced, N mineralized, total N, organic C, microbial biomass, microbial P and phosphatase comprising one group and arylsulphatase, min-N flush, urease and nitrification index comprising the other group. Protease activity and soil pH were not strongly associated with each other or the other groups.     

Decomposition of Zn-rich Arabidopsis halleri Litter in Low and High Metal Soil in the Presence and Absence of EDTA

Hyperaccumulating plants are increasingly investigated in combination with EDTA addition to soil for phytoremediation of heavy metal contaminated soils. A 60-day incubation experiment was carried out to investigate the effects of heavy metal release during the decomposition of Zn-rich (15.7 mg g^?1 dry weight) Arabidopsis halleri litter on C mineralization, microbial biomass C, biomass N, ATP, and adenylate energy charge (AEC). These effects were investigated in two soils with different Zn, Cu, and Pb levels, with and without EDTA addition to soil. The sole addition of Zn-rich A. halleri litter to the two soils did not increase the contents of NH₄NO₃ extractable Zn, only with the combined additions of EDTA and litter was there a considerable increase, being equivalent to three times the added amount in the low metal soil and to 50% in the high metal soil. Litter amendment increased the CO₂ evolved; being equivalent to 44% of the added C in the two soils, but EDTA addition had no significant effect on CO₂ evolution. Litter amendment resulted also in an 18% increase in microbial biomass C, 27% increase in ATP and 6% increase in AEC in the two soils, but EDTA had again no effect on these indices at both metal levels. In contrast, the sole addition of litter had no effect on microbial biomass N, but EDTA addition increased microbial biomass N on average by 49%. The application of EDTA for chelate-assisted phytoextraction should in the future consider the risk of groundwater pollution, which is intensified by resistance of EDTA to microbial decomposition.     

Soil biological properties of a montane forest sere: Corroboration of Odum's postulates

Changes in organic C content, N component pools, Shannon-Weaver diversity index (H′) of microbial populations, nitrification potential, and ATP and dehydrogenase activities were examined in soils along a montane meadow-aspen-fir-spruce sere.Along the sere organic C increased from 2.15 to 26.8%, total N from 0.13 to 0.98%, C: N ratios from 17 to 27, total NH₄⁺ from 103 to 850 μg g^?1, total NH₄⁺:NO₃^? ratios from 69 to 326, and microbial diversity index, H′, from 0.87 to 1.28. Coefficients of determination, r², for H′ vs organic C and total N in A-horizons, were 0.99 and 0.98, respectively, and H′ vs combined O- and A-horizons 0.68 and 0.70, respectively, indicating the presence of different microbial communities in the mineral and forest floor soils. Radiocarbon dating of humic acids and humin showed the longest mean residence times (920 and 1050 yr BP) in the meadow soils, suggesting a more efficient organic matter turnover and selective accumulation of recalcitrant organic components than in soils of more mature stages. The ATP content and dehydrogenase activity values were not statistically different in the forest sequence soils. Rates of nitrification potentials measured in vitro increased along the sere in the surface soils.Information obtained from seral soil variables supported hypothesized successional trends relating to organic matter content, species diversity, nutrient cycling, nutrient exchange rate and nutrient conservation. Nitrification potentials of soils, however, contradicted the postulate that nutrient conservation increases as an ecosystem matures.     

Estimation of microbial biomass and activity in soil using microcalorimetry

Relationships between the rate of heat output from soil, the rate of respiration and the soil microbial biomass were investigated for 25 soils from northern Britain. The rate of heat output, measured in a Calvet microcalorimeter at 22°C, correlated well with the rate of carbon dioxide respiration. The average amount of heat evolved per cm³ of gas respired. 21.1 J cm^?3, suggests that the biomass metabolism was largely aerobic. The rate of heat output per unit of total microbial biomass was remarkably uniform over a wide range of soils, but showed differences depending upon whether the soil had been stored or amended. Mineral soils that had been stored at 4°C had the lowest heat output, 12.0 mW g^?1 biomass C, compared with a mean of 20.4 mW g^?1 biomass C for freshly-collected soils. Amendment with glucose (0.5% w/w) caused an immediate increase in respiration and heat output, up to 59.4 mW g^?1 biomass C for stored soils and 188.2 mW g^?1 biomass C for freshly collected soils. There was a consistent relationship between the biomass and the rate of heat output from freshly collected and amended mineral and organic soils which gave a linear fit using log transformed data: y= 0.6970+ 1.025x (r= 0.98, P < 0.001) (y=log₁₀ biomass C, μgC g^?1; x=log₁₀ rate of heat output at 22°C, μW g^?1). The overall relationship between biomass and the rate of heat output for all the amended samples was: 1 g biomass C= 180.05 ± 34.61 mW.     

Microbial biomass and microbial C:N ratio in bulk soil and buried bags for evaluating in situ net N mineralization in agricultural soils

The in situ net nitrogen mineralization (N_net) was estimated in five agricultural soils under different durations of organic farming by incubating soil samples in buried bags. Simultaneously, soil microbial C and N was determined in buried bags and in bulk soil under winter wheat and after harvest. The aim was to check for variations in soil microbial biomass contents and microbial C:N ratios during the incubation period, and their importance for N_net rates. Microbial C and N contents were highest in soils that had been organically farmed for 41 years, whereas N_net rates were highest in a short‐term organically managed soil that had been under grassland use until 36 years ago. The mean coefficient of variation in the bulk soil for microbial C estimates ranged from 5 to 12 %. Microbial N contents were similar inside buried bags and in the bulk soil at the end of the incubation periods. Under winter wheat during the incubation period until harvest, microbial C contents and microbial C:N ratios (in 10—27 cm depth only) decreased more strongly inside buried bags than in the bulk soil. Following harvest of winter wheat and ploughing, microbial biomass increased while in situ N_net decreased, presumably due to N immobilization. The N_net rates were not correlated with microbial N contents or changes in microbial N contents inside buried bags. At the end of the vegetation period of winter wheat, N_net rates were negatively correlated with microbial C:N ratios. Because these ratios concurrently decreased more inside buried bags than in the bulk soil, the N_net estimates of the buried bag method may differ from the N_net rates in the bulk soil at that time.     

Interference from plant roots in the estimation of soil microbial ATP,C, N and P

Excised, solution-grown roots of maize or ryegrass added to two pasture soils at the rate of 6.0mg g^?1 and 13.8 mg g^?, respectively, increased the flush (fumigated minus control values) of CO₂-C by up to 1.89-fold, KCl extractable N by up to 1.88-fold, and NaHCO₃ extractable P by 3.28-fold. The ATP content of the soil was increased by up to 1.42-fold. Because of high variability the effect of the roots on the C and N flushes was not significant at P < 0.05.Incubation of the root-amended soils for 7 days at 25°C prior to fumigation much decreased the contribution from the roots to the C and N flush, and to the ATP content. There was, however, still a large significant effect of the roots on the P-flush, this being up to 3 times greater than the equivalent soil without roots.In soil samples with a high viable root density (> 6mg g^?1) such as may occur in dense pastures, greenhouse pot experiments or rhizosphere soil samples, it is recommended that they be incubated for 7 days prior to fumigation and analyses. Without such prior incubation there is the risk that root material may be included in the “microbial” biomass estimations.     

The influence of tillage on the proportion of organic carbon and nitrogen in the microbial biomass of medium-textured soils in a humid climate

Summary Microbial biomass C and N respond rapidly to changes in tillage and soil management. The ratio of biomass C to total organic C and the ratio of mineral N flush to total N were determined in the surface layer (0–5 cm) of low-clay (8–10%), fine sandy loam, Podzolic soils subjected to a range of reduced tillage (direct drilling, chisel ploughing, shallow tillage) experiments of 3–5 years' duration. Organic matter dynamics in the tillage experiments were compared to long-term conditions in several grassland sites established on the same soil type for 10–40 years. Microbial biomass C levels in the grassland soils, reduced tillage, and mouldboard ploughing treatments were 561, 250, and 155 g g^-1 soil, respectively. In all the systems, microbial biomass C was related to organic C (r=0.86), while the mineral N flush was related to total N (r=0.84). The average proportion of organic C in the biomass of the reduced tillage soils (1.2) was higher than in the ploughed soils (0.8) but similar to that in the grassland soils (1.3). Reduced tillage increased the average ratio of mineral N flush to total soil N to 1.9, compared to 1.3 in the ploughed soils. The same ratio was 1.8 in the grassland soils. Regression analysis of microbial biomass C and percent organic C in the microbial biomass showed a steeper slope for the tillage soils than the grassland sites, indicating that reduced tillage increased the microbial biomass level per unit soil organic C. The proportion of organic matter in the microbial biomass suggests a shift in organic matter equilibrium in the reduced tillage soils towards a rapid, tillage-induced, accumulation of organic matter in the surface layer.     

Estimation of the adenylate energy charge in unamended and amended agricultural soils

To determine relatively low concentrations of adenine nucleotides in agricultural soils a NaHCO₃-based extradant was developed and compared with the trichloroacetic acid-paraquat-phosphate extradant. The new medium, consisting of chloroform, sodium bicarbonate, phosphate and adenosine (pH 8.0) gave soil extracts which could be investigated without further neutralization and dilution. ATP was measured directly in the soil extracts by the luciferin-luciferase system. ADP and AMP were estimated after their enzymatic conversion to ATP by standard methods. The quantities of nucleotides corrected for recovery of standards were used to calculate the adenylate energy charge (AEC) from the formula AEC = [ATP] + 1/2[ADP]/[ATP] + [ADP] + [AMP], The AEC was estimated in six unplanted soils from agricultural fields. A very similar energy charge of 0.3-0.4 was found in all soils sampled which indicates a low metabolic activity of the soil population. Two other soils with a pronounced difference in biomass-C content were used to investigate the influence of different amendments on the AEC. In an experiment with low glucose supplements up to 500 μg C g^?1 soil, the soil with the low biomass-C (a cambisol) showed a distinct increase of the AEC from 0.34 to 0.50, whereas the soil with the high biomass-C content (a phaeozem) increased its AEC only slightly from 0.32 to 0.37. In another experiment with high glucose supplements the phaeozem reached its maximum AEC value of 0.56 after the addition of 4000 μg Cg^?1 soil. An amendment with 8000 μg C g^?1 soil gave no further increase. In the combisol the addition of 1000 μg C g^?1 soil increased the AEC to 0.61. Higher supplements gave only a slight further increase to a maximum value of 0.67 after the addition of 8000 μg C g^?1 soil. The same AEC value was reached when the cambisol was amended with a mixture of organic substrates at a concentration of 10,000 μg C g^?1 soil.     

Adenylates in the soil microbial biomass at different temperatures

Five soils from temperate sites (Germany; 2 arable and 3 grassland) were incubated aerobically at 5, 10, 15, 20, 25, 35, and 40 °C for 8 days. Soils were analysed for soil microbial biomass C, biomass N, AMP, ADP, and ATP to determine whether the increase in the ATP-to-microbial biomass C ratio with increasing temperature was either due to an increase in the adenylate energy charge (AEC) or de novo synthesis of ATP, or both. Around 80% of the variance in microbial biomass C and biomass N was explained by differences in soil properties, only 7% by the temperature treatments. Averaging the data of all 5 soils for each incubation temperature, the microbial biomass C content decreased with increasing temperature from 15 to 40 °C continuously by 2.5 μg g⁻¹ soil °C⁻¹ after 8-days' incubation. However, this decrease was not accompanied by a similar decrease in microbial biomass N. The average microbial biomass C/N ratio was 6.8. Between 54 and 76% of the variance in AMP, ADP, ATP and the sum of adenylates was explained by differences in soil properties and between 14 (ADP) and 27% (ATP) by the temperature treatments. However, temperature effects on AMP and ADP were variable and inconsistent. In contrast, ATP and consequently also the sum of adenylates increased continuously from 5 to 30 °C followed by a decline to 40 °C. The AEC showed similarly a small, but significant increase with increasing temperature from 0.73 to 0.85 at 30 °C. Consequently, the majority of the variance, i.e. roughly 60% in AEC values, but also in ATP-to-microbial biomass C ratios was explained by the incubation temperature. The mean ATP-to-microbial biomass C ratio increased from 4.7 μmol g⁻¹ at 5 °C to a 2.5 fold maximum of 12.0 μmol g⁻¹ at 35 °C. This increase was linear with a rate of 0.26 μmol ATP g⁻¹ microbial biomass C °C⁻¹. The energy for the extra ATP produced during temperature increase is probably derived from an accelerated turnover of endocellular C reserves in the microbial biomass.     

Response of soil C:N:P stoichiometry,organic carbon stock,and release to wetland grasslandification in Mu Us Desert

Purpose

Wetlands in Mu Us Desert have severely been threatened by grasslandification over the past decades. Therefore, we studied the impacts of grasslandification on soil carbon (C):nitrogen (N):phosphorus (P) stoichiometry, soil organic carbon (SOC) stock, and release in wetland-grassland transitional zone in Mu Us Desert.

Materials and methods

From wetland to grassland, the transition zone was divided into five different successional stages according to plant communities and soil water conditions. At every stage, soil physical and chemical properties were determined and C:N:P ratios were calculated. SOC stock and soil respirations were also determined to assess soil carbon storage and release.

Results and discussion

After grasslandification, SOC contents of top soils (0–10 cm) decreased from 100.2 to 31.79 g kg^?1 in June and from 103.7 to 32.5 g kg^?1 in October; total nitrogen (TN) contents of top soils (0–10 cm) decreased from 3.65 to 1.85 g kg^?1 in June and from 6.43 to 3.36 g kg^?1 in October; and total phosphorus (TP) contents of top soils (0–10 cm) decreased from 179.4 to 117.4 mg kg^?1 in June and from 368.6 to 227.8 mg kg^?1 in October. From stages Typha angustifolia wetland (TAW) to Phalaris arundinacea L. (PAL), in the top soil (0–10 cm), C:N ratios decreased from 32.2 to 16.9 in June and from 19.0 to 11.8 in October; C:P ratios decreased from 1519.2 to 580.5 in June and from 19.0 to 11.8 in October; and N:P ratios decreased from 46.9 to 34.8 in June and changed from 34.9 to 34.0 in October. SOC stock decreased and soil respiration increased with grasslandification. The decrease of SOC, TN, and TP contents was attributed to the reduction of aboveground biomass and mineralization of SOM, and the decrease of soil C:N, C:P, and N:P ratios was mainly attributed to the faster decreasing speeds of SOC than TN and TP. The reduction of aboveground biomass and increased SOC release led by enhanced soil respiration were the main reasons of SOC stock decrease.

Conclusions

Grasslandification led to lowers levels of SOC, TN, TP, and soil C:N, C:P, and N:P ratios. Grasslandification also led to higher SOC loss, and increased soil respiration was the main reason. Since it is difficult to restore grassland to original wetland, efficient practices should be conducted to reduce water drainage from wetland to prevent grasslandification.

     

Essai de correlation entre proprietes biochimiques d'un sol salsodique et sa biomasse

In order to study the influence of salinity on the biological activity of soils, experiments were performed in a saline alkaline soil from Tunisia (mediterranean semi-arid climate) and compared with results of similar experiments performed in a pelosol from a semi-continental climate (Lorraine, France). Both soils had received ¹⁴C-labelled maize straw.The microbial biomass was estimated by a modified Jenkinson's method and also by measurements of ATP content. The microbial activity was determined by measurements of total and ¹⁴CO₂ evolved.The results have shown an inverse correlation between the salinity determined by electrical conductivity and the biomass estimations and its activity. The higher ATP con tent (141.5 ng · 100 g^?1 soil) was observed in the pelosol and the lower (99.4 ng · 100 g^?1) in the saline soil. Simultaneously and respectively in the pelosol and the saline soil the biological carbon evolved was 114 and 54 mgC 100 g^?1 soil and the average rate of ¹⁴C mineralization was 0.82 and 0.45 mgC · 100 g^?1 soil.Results have also shown that CO₂ evolved after sterilization and reinoculation is not only provided by mineralization of microbial biomass during fumigation but also from interaction between organic-matter and CHCl₃; this interaction is more intense in the saline soil.