Influence of salts on the microbial activities in arid and semi-humid soils.

The influence of salt mixtures consisting of Ca(H2PO4)2, trace elements, CaSO4, CaCO3, Na2CO3, NaCl and K2SO4 in different combinations on the nitrifying power, evolution of carbon dioxide and the total number of bacteria was studied in arid soils (sandy and alluvial) and semi-humid ones (chernozem and rendzina). Salt mixtures comprising of either mono-calcium phosphate or sodium chloride showed highly inhibiting action on the studied microbial activities in sandy, alluvial and chernozem soils, whilst mono-calcium phosphate stimulated the heterotrophs of rendzina. Trace elements stimulated the autotrophs of the clay soils. The other different salts mixtures acted according to the salt combination and nature of the microbial activity.     

Salt dependence, kinetic properties and catalytic mechanism of N-formylmethanofuran:tetrahydromethanopterin formyltransferase from the extreme thermophile Methanopyrus kandleri.

N-Formylmethanofuran(CHO-MFR):tetrahydromethanopterin(H4MPT) formyltransferase (formyltransferase) from the extremely thermophilic Methanopyrus kandleri was purified over 100-fold to apparent homogeneity with a 54% yield. The monomeric enzyme had an apparent molecular mass of 35 kDa. The N-terminal amino acid sequence of the polypeptide was determined. The formyltransferase was found to be absolutely dependent on the presence of phosphate or sulfate salts for activity. The ability of salts to activate the enzyme decreased in the order K2HPO4 > (NH4)2SO4 > K2SO4 > Na2SO4 > Na2HPO4. The salts KCl, NaCl and NH4Cl did not activate the enzyme. The dependence of activity on salt concentration showed a sigmoidal curve. For half-maximal activity, 1 M K2HPO4 and 1.2 M (NH4)2SO4 were required. A detailed kinetic analysis revealed that phosphates and sulfates both affected the Vmax rather than the Km for CHO-MFR and H4MPT. At the optimal salt concentration and at 65 degrees C, the Vmax was 2700 U/mg (1 U = 1 mumol/min), the Km for CHO-MFR was 50 microM and the Km for H4MPT was 100 microM. At 90 degrees C, the temperature optimum of the enzyme, the Vmax was about 2.5-fold higher than at 65 degrees C. Thermostability as well as activity of formyltransferase was dramatically increased in the presence of salts, 1.5 M being required for optimal stabilization. The efficiency of salts in protecting formyltransferase from heat inactivation at 90 degrees C decreased in the order K2HPO4 = (NH4)2SO4 > KCl = NH4Cl = NaCl > Na2SO4 > Na2HPO4. The catalytic mechanism of formyltransferase was determined to be of the ternary-complex type. The properties of the enzyme from M. kandleri are compared with those of formyltransferase from Methanobacterium thermoautotrophicum, Methanosarcina barkeri and Archaeoglobus fulgidus.     

Comparative Toxicities of Salts on Microbial Processes in Soil

Soil salinization is a growing threat to global agriculture and carbon sequestration, but to date it remains unclear how microbial processes will respond. We studied the acute response to salt exposure of a range of anabolic and catabolic microbial processes, including bacterial (leucine incorporation) and fungal (acetate incorporation into ergosterol) growth rates, respiration, and gross N mineralization and nitrification rates. To distinguish effects of specific ions from those of overall ionic strength, we compared the addition of four salts frequently associated with soil salinization (NaCl, KCl, Na₂SO₄, and K₂SO₄) to a nonsaline soil. To compare the tolerance of different microbial processes to salt and to interrelate the toxicity of different salts, concentration-response relationships were established. Growth-based measurements revealed that fungi were more resistant to salt exposure than bacteria. Effects by salt on C and N mineralization were indistinguishable, and in contrast to previous studies, nitrification was not found to be more sensitive to salt exposure than other microbial processes. The ion-specific toxicity of certain salts could be observed only for respiration, which was less inhibited by salts containing SO₄²⁻ than Cl⁻ salts, in contrast to the microbial growth assessments. This suggested that the inhibition of microbial growth was explained solely by total ionic strength, while ion-specific toxicity also should be considered for effects on microbial decomposition. This difference resulted in an apparent reduction of microbial growth efficiency in response to exposure to SO₄²⁻ salts but not to Cl⁻ salts; no evidence was found to distinguish K⁺ and Na⁺ salts.     

Comparative effects of varying levels of chlorides and sulphates of sodium,potassium, calcium,and magnesium on ammonification and nitrification during incubation of soil

Summary The effect of chlorides and sulphates of sodium, potassium, calcium, and magnesium, added at 01.% to 2.0% sodium chloride-equivalent (soil basis), on nitrogen mineralization and nitrification during incubation (3 weeks, 30°C) of soil was studied. For the chloride series the critical level for virtually complete suppression of nitrification was between 0.5% and 1.0% of the added salts. Nitrogen mineralization was reduced only where 1–2% of salts were added. In the sulphate series nitrogen mineralization and nitrification were reduced to a fair extent only by the 2% level of sodium sulphate, the other sulphates having little or no effect on these processes. At some levels the sulphates and chlorides of all cations, except sodium, resulted in a small but significant increase in nitrogen mineralization.     

Impact of long and short term irrigation of a sodic soil with distillery effluent in combination with bioamendments

The study reports the effects of irrigation of a sodic soil with post methanation effluent (PME) of a distillery. Impact of long term effluent irrigation in the field (10 years) and short term effluent irrigation using different doses of PME in the laboratory (30 days) was studied in combination with three bioamendments i.e. farmyard manure, brassica residues and rice husk. Impact on various soil properties like EC, pH, total organic carbon (TOC), total Kjeldahl nitrogen (TKN), available phosphorus, exchangeable K, Na, Ca, Cl, microbial population and soil enzyme activities were studied. Long term application of PME proved useful in significantly increasing TOC, TKN, K, P and soil enzymatic activities in the soil but tended to build up harmful concentration of Na, that could be chelated by bioamendments. In short terms studies, application of 50% PME along with bioamendments proved to be the most useful in improving the properties of sodic soil and also favoured successful germination and improved seedling growth of pearl millet.     

The radiation response of cultured mammalian V79-S171 cells exposed to a wide concentration range of sulphate salt solutions.

The radiation response of Chinese hamster cells (V79) exposed to a wide concentration range of Li2SO4, Na2SO4 or K2SO4 has been examined and compared with the radiation response of cells treated in an identical manner with LiCl, NaCl, or KCl solutions. At hypotonic salt concentrations, cells were radiosensitized by both the chloride and sulphate salts. At high salt concentrations, approximately greater than 0.9 M, a radioprotective effect was observed with both chloride and sulphate salts. At intermediate salt concentrations from about 0.2 to 0.9 M, the cells that were treated with the sulphate salt solutions were radioprotected; cells treated with chloride salt solutions were radiosensitized. The difference in radiation response was attributed to the difference in anions for the two types of salts used.     

Osmotic and specific ion effects on the germination of Prosopis strombulifera

BACKGROUND AND AIMS: Salinity can affect germination of seeds either by creating osmotic potentials that prevent water uptake or by toxic effects of specific ions. Most studies have only used monosaline solutions, although these limit the extent to which one can interpret the results or relate them to field conditions. The aim of this work was to evaluate the germination of Prosopis strombulifera seeds under increasing salinity by using the most abundant salts in central Argentina in monosaline or bisaline iso-osmotic solutions, or in solutions of mannitol and polyethylene glycol. METHODS: Seeds were allowed to germinate under controlled conditions in a germination chamber at 30 +/- 1 degrees C and at 80 % r.h. Salinizing agents were KCl, NaCl, Na(2)SO(4), K(2)SO(4), NaCl + Na(2)SO(4) and KCl + K(2)SO(4) and osmotic agents were polyethylene glycol 6000 and mannitol. Treatments for all osmotica consisted of 0.0, -0.4, -0.8, -1.2, -1.5, -1.9 and -2.2 MPa solutions. KEY RESULTS: The percentage of germination decreased as salinity increased. SO(4)(2-) in monosaline solutions, with osmotic potentials -1.2 MPa and lower, was more inhibitory than Cl(-) at iso-osmotic concentrations. This SO(4)(2-) toxicity was alleviated in salt mixtures and was more noticeable in higher concentrations. K(+) was more inhibitory than Na(+) independently of the accompanying anion. CONCLUSIONS: Different responses to different compositions of iso-osmotic salt solutions and to both osmotic agents indicate specific ionic effects. This study demonstrates that the germination of P. strombulifera is strongly influenced by the nature of the ions in the salt solutions and their interactions. Comparative studies of Cl(-) and SO(4)(2-) effects and the interaction between SO(4)(2-) and Cl(-) in salt mixtures indicate that extrapolation of results obtained with monosaline solutions in the laboratory to field conditions can be speculative.     

Microbial mineralization of VC and DCE under different terminal electron accepting conditions

Production of 14CO2 from [1,2-14C] dichloroethene (DCE) or [1,2-14C] vinyl chloride (VC) was quantified in aquifer and stream-bed sediment microcosms to evaluate the potential for microbial mineralization as a pathway for DCE and VC biodegradation under aerobic, Fe(III)-reducing, SO4-reducing, and methanogenic conditions. Mineralization of [1,2-14C] DCE and [1,2-14C] VC to 14CO2 decreased under increasingly reducing conditions, but significant mineralization was observed for both sediments even under anaerobic conditions. VC mineralization decreased in the order of aerobic > Fe(III)-reducing > SO4-reducing > methanogenic conditions. For both sediments, VC mineralization was greater than DCE mineralization under all electron-accepting conditions examined. For both sediments, DCE mineralization was at least two times greater under aerobic conditions than under anaerobic conditions. Although significant microbial mineralization of DCE was observed under anaerobic conditions, recovery of 14CO2 did not differ substantially between anaerobic treatments.     

长穗薄冰草（Thinopyrum ponticum）对盐碱胁迫的生理响应

实验采用不同浓度（以干土重0.3%、0.5%、0.7%和0.9%计）Na2SO4、NaCl、NaHCO3、Na2CO3,Na2SO4：NaCl=1：1、NaHCO3：Na2CO3=1：1和Na2SO4：NaCl：NaHCO3：Na2CO3=1：1：1：1对长穗薄冰草进行胁迫,研究长穗薄冰草对盐碱胁迫的生理响应.结果表明：根系活力、SOD活性随盐碱浓度的增加逐渐下降,脯氨酸含量呈上升趋势,叶绿素含量除Na2SO4处理组外,呈先上升后下降的趋势.其中碱性盐（NaHCO3、Na2CO3、NaHCO3：Na2CO3=1：1、Na2SO4：NaCl：NaHCO3：Na2CO3=1：1：1：1）对长穗薄冰草的胁变效应较中性盐（Na2SO4、NaCl、Na2SO4：NaCl=1：1）大,以Na2SO4处理组对长穗薄冰草的影响最小,0.7% Na2CO3是长穗薄冰草正常生长的临界浓度.     

盐碱混合生态条件的人工模拟及其对羊草胁迫作用因素分析

将中性盐NaCl和Na2SO4,碱性盐NaHCO3和Ｎa2CO3按不同比例混合,模拟出３０种盐度和pH各不相同的盐碱生态条件,并对羊草苗进行盐碱混合胁迫处理,测定其日相对生长率（ＲＧＲ）等７项胁变指标,用数学方法分析盐度,缓冲量等各种胁迫因素与诸项胁变指标间的相互关系,结果表明：30种处理均匀覆盖了总盐度50-350mmol/L,pH7.14-10.81范围内的各种盐碱条件,用盐度,缓冲量,pH和[Cl^-]即可代表盐碱混合胁迫的所有胁迫作用因素,诸胁变指标与这4因素间均具有高度线性相关性,4因素对胁变的贡献明显不同,其中缓冲量和盐度是决定性的主导因素,pH和[Cl^-]的作用明显次之,有时甚至可以忽略,不同胁变指标与各因素的关系也有不同。分析结果表明,对于盐碱混合胁迫来说,以盐度加缓冲量代表总胁强较为合理。     

Effect of SO2 and bisulfite on heterotrophic activity in an acid soil.

Glucose oxidation was inhibited in a forest soil (pH 4.01) previously exposed by 1.0 microliter of SO2 per liter, the extent of inhibition and the decline in pH being directly related to the length of exposure. The phase of rapid CO2 evolution in protein hydrolysate-amended soil previously treated with 5.0 microliter of SO2 per liter for 24 h or 1.0 microliter/liter for 48 h was delayed, but the degradation of the amino acid mixture then proceeded rapidly. Bacterial numbers in soil incubated for 48 h with 1.0 microliter of SO2 per liter were reduced, but the bacteria grew rapidly if glucose or an amino acid mixture was added after the exposure period. Low levels of bisulfite inhibited amino acid decomposition in soil at pH 3.89, but the effect was less pronounced in soil at pH 4.01. Comparable levels of sulfate were not toxic to carbon mineralization. Approximately 1.0 microgram of bisulfite S and about 20 microgram of sulfate S per g of soil appeared when the soil was treated with 1.0 microliter of SO2 per liter for 48 h. Bisulfite added to the soil disappeared readily. The possible ecological significance of the findings is discussed.     

Effect of SO2 and bisulfite on heterotrophic activity in an acid soil.

Glucose oxidation was inhibited in a forest soil (pH 4.01) previously exposed by 1.0 microliter of SO2 per liter, the extent of inhibition and the decline in pH being directly related to the length of exposure. The phase of rapid CO2 evolution in protein hydrolysate-amended soil previously treated with 5.0 microliter of SO2 per liter for 24 h or 1.0 microliter/liter for 48 h was delayed, but the degradation of the amino acid mixture then proceeded rapidly. Bacterial numbers in soil incubated for 48 h with 1.0 microliter of SO2 per liter were reduced, but the bacteria grew rapidly if glucose or an amino acid mixture was added after the exposure period. Low levels of bisulfite inhibited amino acid decomposition in soil at pH 3.89, but the effect was less pronounced in soil at pH 4.01. Comparable levels of sulfate were not toxic to carbon mineralization. Approximately 1.0 microgram of bisulfite S and about 20 microgram of sulfate S per g of soil appeared when the soil was treated with 1.0 microliter of SO2 per liter for 48 h. Bisulfite added to the soil disappeared readily. The possible ecological significance of the findings is discussed.     

Testing of some assumptions about biodegradability in soil as measured by carbon dioxide evolution.

Conversion to CO2 upon incubation in aerobic soil is one of the standard test procedures to assess biodegradability. It may be measured with unlabeled test compounds in biometer flasks. In this case, the background CO2 evolution by unamended soil is subtracted from the CO2 evolution by the amended soil and the resulting net CO2 evolution becomes the measure of biodegradation. Alternately, 14CO2 release from radiocarbon substrates is measured to assess biodegradability. Both approaches measure ultimate (complete) biodegradation and bypass the theoretical and technical limitations of residue analysis. This report examines the underlying assumptions that, except for carbon content, conversion percentage to CO2 is relatively independent of chemical composition, that CO2 production is proportional to the amount of added test compound, and that the background CO2 evolution of the soil is not influenced by the test substance. Work with unlabeled and radiolabeled substrates proved the first two assumptions to be essentially correct. However, more than half of net CO2 production may represent the mineralization of biomass and soil organic matter, some of it unrelated to the test compound. The soil microbial community in its nongrowing steady state appears to convert a much lower percentage of a radiocarbon substrate to 14CO2 than a growing soil community that responds to a substantial substrate addition. These findings may help to improve test methods and may aid in the interpretation of test results.     

Effect of salts and organic solvents on the activity of Halobacterium cutirubrum catalase

Catalase in extracts of the extreme halophile Halobacterium cutirubrum exhibits up to threefold stimulation by 0.5 to 1.5 m monovalent salts and by 0.1 m divalent salts. Above these concentrations, inhibition of enzyme activity is observed. The inhibitory effect, and to some extent the stimulation, is salt-specific; the effectiveness of a salt in inhibiting enzyme activity depends on both cation and anion. Thus, the order of effectiveness is MgCl(2) > LiCl > NaCl > KCl > NH(4)Cl, and LiCl > LiNO(3) > Li(2)SO(4). The magnitude of enzyme inhibition for the salts tested is positively correlated with their molar vapor pressure depression in aqueous solution. Stimulation of enzyme activity was observed when one salt was added at its optimal concentration in the presence of inhibiting concentrations of another salt, indicating that the effect on the enzyme is not due to changing water activity but probably to enzyme-salt interaction. Aqueous solutions of ethylene glycol, glycerol, and dimethyl sulfoxide containing no ions influence enzyme activity in the same manner as do salts.     

Soil C and N availability determine the priming effect: microbial N mining and stoichiometric decomposition theories

The increasing input of anthropogenically derived nitrogen (N) to ecosystems raises a crucial question: how does available N modify the decomposer community and thus affects the mineralization of soil organic matter (SOM). Moreover, N input modifies the priming effect (PE), that is, the effect of fresh organics on the microbial decomposition of SOM. We studied the interactive effects of C and N on SOM mineralization (by natural ¹³C labelling adding C₄‐sucrose or C₄‐maize straw to C₃‐soil) in relation to microbial growth kinetics and to the activities of five hydrolytic enzymes. This encompasses the groups of parameters governing two mechanisms of priming effects – microbial N mining and stoichiometric decomposition theories. In sole C treatments, positive PE was accompanied by a decrease in specific microbial growth rates, confirming a greater contribution of K‐strategists to the decomposition of native SOM. Sucrose addition with N significantly accelerated mineralization of native SOM, whereas mineral N added with plant residues accelerated decomposition of plant residues. This supports the microbial mining theory in terms of N limitation. Sucrose addition with N was accompanied by accelerated microbial growth, increased activities of β‐glucosidase and cellobiohydrolase, and decreased activities of xylanase and leucine amino peptidase. This indicated an increased contribution of r‐strategists to the PE and to decomposition of cellulose but the decreased hemicellulolytic and proteolytic activities. Thus, the acceleration of the C cycle was primed by exogenous organic C and was controlled by N. This confirms the stoichiometric decomposition theory. Both K‐ and r‐strategists were beneficial for priming effects, with an increasing contribution of K‐selected species under N limitation. Thus, the priming phenomenon described in ‘microbial N mining’ theory can be ascribed to K‐strategists. In contrast, ‘stoichiometric decomposition’ theory, that is, accelerated OM mineralization due to balanced microbial growth, is explained by domination of r‐strategists.     

Action of exogenous potassium and calcium ions on in vitro metacyclogenesis in Trypanosoma cruzi.

The cations Ca2+ and K+ and the anions Cl-, HCO3-, and PO4- were studied for their contribution to metacyclic trypomastigote formation of Trypanosoma cruzi in starvation media consisting of phosphate-buffered saline (PBS) + 10 mM proline + 10 mM sodium acetate as well as one of the following salts: 0.035% NaHCO3 (PBSNPA), 0.035% K2CO3 (PBSKPA) or 0.035% K2HPO4 (PBSPPA). Isolates CL and DM28c were activated to transform with 5% CO2 and the percent metacyclogenesis determined after incubation for 96 h in PBS starvation media. Maximal metacyclogenesis was found with CaCl2 and KCl. In the presence of K+, the percent transformation was highest with the phosphate salt, followed by the carbonate and the chloride salts. Cells incubated in PBSNPA and the cationic ionophores A23187 (5 x 10(-6) M), lasalocid (5 x 10(-6) M), and valinomycin (10(-8) M) do not survive; addition of 2 mM CaCl2 or 17 mM KCl to DM28c cells, reversed the lethal action of the ionophores permitting differentiation into metacyclic forms. The addition of CaCl2 to CL cells incubated in ionophores abrogated the lethal effect of the ionophores but transformation was significantly different than in control preparations. Adding KCl to ionophore incubated cells resulted in normal levels of transformation except in the case of valinomycin. DM28c and CL cells incubated in PBSKPA show significantly greater metacyclogenesis in the presence of 5 mM EGTA. These results indicate that exogenous concentrations of several cations and anions significantly influence T. cruzi metacyclogenesis and that the degree of response by the parasite to free ion levels may be strain dependent.     

不同施肥处理对玉米秸秆碳氮比及其矿化特性的影响

以两个长期定位试验不同施肥处理玉米秸秆为对象,采用室内培养试验研究了其碳、氮养分在土壤中的矿化特性.结果表明：与未施肥处理相比,施用化肥（NPK）或化肥与有机肥配施（MNPK）处理明显增加了玉米秸秆的氮素含量,降低了其C/N.不同处理秸秆碳、氮矿化量和被微生物固持的碳、氮量因培养时期不同而异,NPK、MNPK和240 kg N·hm^-2处理秸秆在培养期间碳的矿化率显著高于相应不施肥处理;60 d培养期结束后,NPK处理秸秆的有机碳矿化量最大,占加入总有机碳的13.24%.各施肥处理玉米秸秆施入土壤后引起的土壤矿质氮固持量均较不施肥秸秆低,其中MNPK处理最低.施用秸秆增加了土壤微生物的代谢熵（qCO₂）,但不同处理间qCO₂的差异较小;各处理土壤微生物生物量碳、氮含量因培养时期不同而异.因此,生产中利用秸秆时应考虑不同施肥处理秸秆养分含量的差异.     

不同施肥处理对玉米秸秆碳氮比及其矿化特性的影响

以两个长期定位试验不同施肥处理玉米秸秆为对象,采用室内培养试验研究了其碳、氮养分在土壤中的矿化特性.结果表明：与未施肥处理相比,施用化肥（NPK）或化肥与有机肥配施（MNPK）处理明显增加了玉米秸秆的氮素含量,降低了其C/N.不同处理秸秆碳、氮矿化量和被微生物固持的碳、氮量因培养时期不同而异,NPK、MNPK和240 kg N·hm^-2处理秸秆在培养期间碳的矿化率显著高于相应不施肥处理;60 d培养期结束后,NPK处理秸秆的有机碳矿化量最大,占加入总有机碳的13.24%.各施肥处理玉米秸秆施入土壤后引起的土壤矿质氮固持量均较不施肥秸秆低,其中MNPK处理最低.施用秸秆增加了土壤微生物的代谢熵（qCO₂）,但不同处理间qCO₂的差异较小;各处理土壤微生物生物量碳、氮含量因培养时期不同而异.因此,生产中利用秸秆时应考虑不同施肥处理秸秆养分含量的差异.     

Cuticular penetration of potassium salts: Effects of humidity,anions, and temperature

Cuticular penetration of potassium salts across astomatous cuticular membranes isolated from pear and Citrus leaves has been studied. Penetration was a first order process and was greatly affected by humidity and hygroscopicity of salts. Temperature did not significantly influence rates of penetration in the range of 10 – 25 °C. Penetration required dissolution of the salt and this is determined by the point of deliquescence (POD) and humidity. When humidity is above the POD the salt residue on the cuticle dissolves, while below a solid residue is formed and penetration ceases. The POD for K₂CO₃ is 44% at 20 °C and above this humidity salt penetration was possible. Rate constants of penetration increased from 0.022 to 0.045 h^–1 when humidity increased from 50 to 90%. With KCl (POD of 86%) rates were highest at 90% and lower at 100% while with KNO₃ (POD of 95%) and KH₂PO₄ (POD of 97%) highest rates were measured at 100% humidity and at 90% penetration was extremely slow. With KCl, KNO₃ and K₂CO₃ maximum rate constants of penetration across pear CM were around 0.04 – 0.05 h^–1 which correspond to half times of penetration of 14 – 17 h. Rate constants measured with Citrus CM were up to two times higher but response to humidity was similar. The potassium salts studied did not only differ in POD and sensitivity to humidity but also in potassium content, which is highest with K₂CO₃ (57%) and KCl (52%) and much lower with KNO₃ (38%) and KH₂PO₄ (29%). Thus, K₂CO₃ is best suited for foliar applications as rates of penetration were large at 50% humidity and higher, while with the other salts humidity must be 90 – 100% for maximum rates of penetration.     

六盘山林区几种土地利用方式对土壤有机碳矿化影响的比较

 应用土壤培养法,比较分析了六盘山林区天然次生林（杂灌林、山杨（Populus davidanda）和辽东栎（Quercus liaotungensis）林）、农田、草地和人工林（13 a、18 a和25 a华北落叶松（Larix principis-rupprechtii））土壤在30℃和60%田间饱和含水量条件下培养180 d有机碳矿化速率的差异（以180 d累计释放的CO2-C计）。结果显示：农田和草地土壤碳矿化释放的CO2-C含量（180 d释放的gCO2-C·kg-1干土）分别比天然次生林低65%和23%,差异主要在0～40土层;人工林比农田和草地分别高155%和 17%,差异主要在0～70 cm土层。农田土壤碳矿化释放的CO2-C分配比例（即180 d释放CO2-C/土壤 C）比天然次生林平均低12%,草地比天然次生林平均高18%,差异主要在0～40 cm土层;人工林比农田平均高29%,草地比人工林平均高9%,差异主要在0～50 cm土层。不同土地利用方式土壤碳矿化释放的CO2-C含量的差异比其分配比例的差异大。土壤碳矿化释放的CO2-C含量和分配比例总体上都随土层加深而递减。分配比例随土层加深而递减的幅度方面,不同土地利用方式间的差异不大;含量随土层加深而递减的幅度方面,天然次生林和人工林比农田和草地中大;随土层递减的幅度方面,土壤碳矿化释放的CO2-C含量比其分配比例大。这主要由不同土地利用方式土壤碳输入和稳定性等差异所致。结果说明土壤碳矿化速率随天然次生林变成农田或草地而下降,随在农田或草地上造林而增加, 矿化速率变化幅度比分配比例的变化幅度大。另外,土地利用变化也使不同土层土壤碳矿化速率和分配比例差异改变,其中速率改变的幅度比分配比例改变的幅度大。