Comparison of Two Cellulomonas Strains and Their Interaction with Azospirillum brasilense in Degradation of Wheat Straw and Associated Nitrogen Fixation

A mutant strain of Cellulomonas sp. CS1-17 was compared with Cellulomonas gelida 2480 as the cellulolytic component of a mixed culture which was responsible for the breakdown of wheat straw to support asymbiotic nitrogen fixation by Azospirillum brasilense Sp7 (ATCC 29145). Cellulomonas sp. strain CSI-17 was more efficient than was C. gelida in cellulose breakdown at lower oxygen concentrations and, in mixed culture with A. brasilense, it supported higher nitrogenase activity (C₂H₂ reduction) and nitrogen fixation with straw as the carbon source. Based on gravimetric determinations of straw breakdown and total N determinations, the efficiency of nitrogen fixation was 72 and 63 mg of N per g of straw utilized for the mixtures containing Cellulomonas sp. and C. gelida, respectively. Both Cellulomonas spp. and Azospirillum spp. exhibited a wide range of pH tolerance. When introduced into sterilized soil, the Cellulomonas sp.-Azospirillum brasilense association was more effective in nitrogen fixation at a pH of 7.0 than at the native soil pH (5.6). This was also true of the indigenous diazotrophic microflora of this soil. The potential implications of this work to the field situation are discussed.     

有机物料在维持土壤微生物体氮库中的作用

采用室内和田间培养试验,研究了有机物料矿化过程中土壤微生物体氮的变化,测定结果表明,有机物料对矿化过程和微生物体氮的影响,既与有机物料本身性质和组成有关,也与土壤肥力水平和施氮与否有关。加入Ｃ／Ｎ比高的有机物料后,微生物对矿质氮的净固定持续时间长,而加入Ｃ／Ｎ比小的则固定时间短;高肥力土壤上的固定时间比低肥力土壤短。不同有机物料对土壤微生物体氮的影响不同。从加绿豆茎叶、小麦茎叶、未腐解马粪、腐熟马粪、腐熟猪粪到厩肥,土壤微生物体氮依次减小,提供的有效能源物质丰富（如绿豆茎叶）或Ｃ／Ｎ比较高（如小麦茎叶）时影响效果突出。土壤肥力不同,有机物料对微生物体的影响效果不同,在低肥力土壤的效果突出,约为高肥力土壤的４倍,因此,在评价有机物料对土壤微生物体氮的影响时,既考虑有有机物料的性质和组成,也考虑土壤力水平、矿质氮含量和培养时期。     

Effects on straw decay of the herbicides paraquat and glyphosate in combination with nitrogen amendments

The effects of paraquat were studied at 4.7 kg a. i./ha and of glyphosate at 9.4 kg a. i./ha on the weight loss and rate of oxygen uptake by stems of barley straw, incubated on the soil surface for various periods of time, and stems and leaves of wheat straw on the soil surface or covered with a shallow layer of soil. In general, paraquat reduced weight loss and frequently oxygen uptake. Glyphosate normally had no effect but occasionally it was stimulatory. However, in isolated instances, paraquat was inactive and glyphosate slightly inhibitory. Leaves decayed faster than stems. Burial, as well as the addition to straw of leaf protein, Nitrochalk, urea and clover plants increased decomposition in all treatments, but nitrogen amendments were less effective in those with paraquat. For example, urea enhanced weight loss after 21 wk from 19 to 34% of the initial weight in unsprayed wheat straw, from 12 to 24% in paraquat-treated and from 20 to 37% in glyphosate-treated straw, indicating that conditions stimulating decomposition may attenuate but not entirely eliminate the inhibitory effects of paraquat. A repeated addition of nitrogen to straw in various stages of decay increased oxygen uptake in all treatments but least in the paraquat-treated straw, implying that a complete recovery from the initial curtailment of microbial activity, brought about by this herbicide, did not occur. Although the concentration of paraquat used was nine times greater than the minimum recommended for field application, the degree of inhibition observed in these laboratory experiments was probably not sufficiently great to be of marked economic importance.     

Non-symbiotic nitrogen fixation in soil

Summary 1. The fixation of N¹⁵-labeled nitrogen in small vessels of California soil under various conditions of pH, substrate level, oxygen tension, and other soil conditions was observed.2. Nitrate concentrations greater than 1.0–1.5 microequivalents per gram soil were found to suppress nitrogen fixation but not the growth ofAzotobacter.3. Large amounts of nitrogen were fixed when soluble organic substrates (e.g. glucose or sucrose) were added to the soil.4. Moderate fixation also resulted from the inversion of a disc of sod.5. Fixed nitrogen appeared largely in the nitrate and ammonia-amide fractions with that in the nitrate fraction probably representing nitrification of more reduced initial products of fixation.6. Under conditions of these experiments growing grass did not enhance fixation. At higher light intensities, however, such an enhancement might be observed.7. The incorporation of grass cuttings, straw or alfalfa meal into the soil caused only a slight increase in fixation.8. The inoculation of soils with large populations ofAzotobacter did not result in increased fixation.This investigation was supported in part by a contract with the United States Atomic Energy Commission.     

发酵肥与秸杆还田对土壤呼吸,固氮与反硝化作用的影响

土壤中施入不发酵新鲜粪肥时反硝化作用增强,固氮活性明显减弱;当施入发酵肥时反硝化作用较弱,而固氮活性比不发酵肥强。在施发酵肥基础上再进行秸秆还田,土壤呼吸作用增强,反硝化作用进一步减弱,固氮活性提高。在秸秆还田时喷雾接种木霉（Ｔｒｉｃｈｏｄｅｒｍａｋｏｎｉｎｇｉ）４５８—２与固氮菌（Ａｚ．ｖｉｎｅｌａｎｄｉｉ）２３０提高了土壤固氮活性。     

Soybean nodule gas permeability,nitrogen fixation and dirunal cycles in soil temperature

While diurnal cycles in nitrogen fixation rates are sometimes assumed to result from diurnal variation in photosynthetically active radiation, contradicting evidence exists that indicate soil temperature is the primary environmental influence. These studies assessed the significance of temperature on soybean nitrogen fixation under field conditions. Two groups of intact field-grown soybean plants, one at ambient and the other exposed to a 10°C diurnal variation in soil temperature, were nondestructively assayed for acetylene reduction rates. Activity was closely associated with soil temperature (R²=0.85), even when temperature was 12 h out of phase with ambient. Data were also obtained to determine if the effects of rhizosphere temperature on nitrogen fixation are mediated through an effect on the nodule oxygen permeability. Nodule oxygen permeability of intact, aeroponically grown soybean was closely correlated with the diurnal changes in temperature (R²=0.90).     

Effect of oxygen concentration on dinitrogen fixation and volatile fatty acid production by Clostridium butyricum growing in association with fungi on cellulose and on wheat straw

Clostridium butyricum was grown with cellulolytic fungi on the substrates wheat straw and cellulose at a range of oxygen concentrations. The straw was not sterile and was inoculated with Sodaria alcina while the cellulose was sterile and was inoculated with Trichoderma harzianum as examples of cellulolytic organisms. The straw subsequently developed a mixed fungal population. Dinitrogen fixation was only significant at a reduced oxygen concentration: optima being 9.3 and 2.3% O₂ for the straw and cellulose experiments, respectively. The efficiencies of N, fixation were 6 mg N per g straw decomposed and 2.3 mg N per g cellulose decomposed and N, fixation occurred only in the presence of significant cellulolysis. Both acetate and butyrate formation increased as the oxygen concentration decreased. With cellulose as a substrate, their formation correlated with a decrease in pH and an increase in final numbers of Cl. butyricum . The thickness of the anaerobic zone at the aerobic/anaerobic interface was linearly related to the square root of the oxygen concentration at the surface of the interface.     

Nitrogen limitation and nitrogen fixation during alkane biodegradation in a sandy soil.

We investigated nutrient limitations during hydrocarbon degradation in a sandy soil and found that fixed nitrogen was initially a limiting nutrient but that N limitation could sometimes be overcome by N2 fixation. Hydrocarbon biodegradation was examined in an unsaturated sandy soil incubated aerobically at 20 degrees C with propane or butane and various added nutrients. Propane and butane degradation proceeded similarly during the first 3 months of incubation. That is, bacteria in soil amended with N oxidized these hydrocarbons more rapidly than in controls without nutrient additions or in soil with added phosphate or trace minerals. Both propane- and butane-amended soil apparently became N limited after the initial available inorganic N was utilized, as indicated by a decrease in the rates of hydrocarbon degradation. After 3 months, propane and butane degradation proceeded differently. Bacteria in propane-degrading soil apparently remained N limited because propane degradation rates stayed low unless more N was added. In contrast, bacteria in butane-degrading soil appeared to overcome their N limitation because butane degradation rates later increased regardless of whether more N was added. Analyses of total N and acetylene reduction assays supported this apparent surplus of N in butane-amended soil. Total N was significantly (P < 0.01) higher in soil incubated with butane and no N amendments than in soil incubated with propane, even when the latter was amended with N. Acetylene reduction occurred only in butane-amended soil. These results indicate that N2 fixation occurred in butane-amended soil but not in propane-amended soil.     

15N2 incorporation by rhizosphere soil influence of rice variety,organic matter and combined nitrogen

Summary Heterotrophic nitrogen fixation by rhizosphere soil samples from 20 rice cultivars grown under uniform field conditions was estimated employing¹⁵N-tracer technique. Rhizosphere soil samples from different rice cultivars showed striking differences with regard to their ability to incorporate¹⁵N₂. Rhizosphere samples from rice straw-amended (3 and 6 tons/ha) soil exhibited more pronounced nitrogen-fixing activity than the samples from unamended soil; while the activity of the rhizosphere samples from soils receiving combined nitrogen (40 and 80 kg N/ha) was relatively low. However, the inhibitory effect of combined nitrogen was not expressed in the presence of rice straw at 6 tons/ha. Results suggest that plant variety, application of combined nitrogen and organic matter influence the rhizosphere nitrogen fixation.     

土壤有机氮组分的年际变化及其对秸秆还田的响应

阐明土壤有机氮组分的年际变化特征及其对秸秆还田的响应对合理调控土壤有机氮库和土壤可持续利用具有重要意义。在沈阳农田生态系统国家野外科学观测研究站进行田间微区试验(土壤类型为潮棕壤),设置单施氮肥(200 kg N·hm^-2,下同)、50%秸秆还田配施氮肥和100%秸秆还田配施氮肥3个处理,采用Bremner酸水解法对试验第1、3、6、9年的土壤有机氮组分进行分级。结果表明: 氨基酸态氮含量随着耕作年限的增加逐渐提升,提升幅度为39.8%;酸解未知态氮含量提升幅度为10.8%,且在第3年时最高;土壤总氮和其他有机氮组分含量随耕作年限变化不大。相对容易矿化的酸解总氮占土壤总氮的比例随耕作年限的增加逐渐增加,比较稳定的未酸解态氮占土壤总氮的比例随耕作年限的增加逐渐下降,说明随着耕作年限的增加土壤氮素有效性提高,土壤供氮能力增强。与单施氮肥相比,加入秸秆提高了土壤总氮和各酸解态氮含量,秸秆还田量越多,提升效果越明显。秸秆还田对酸解态氮组分的影响主要发生在试验第6、9年,增加的土壤总氮主要为氨基酸态氮和酸解未知态氮,从而提高了土壤中酸解态氮占土壤总氮的比例。秸秆还田能够提升土壤氮库容,提高土壤保氮供氮能力。     

Phytotoxicity from plant residues

Summary Proximity of new wheat straw residues to sown wheat seed has an effect on germination, plant growth and ultimate yield. Decomposition of wheat straw may produce toxins or it may cause immobilization of nitrogen in, or applied to the soil. In pot experiments, it has been shown that germination of wheat was depressed when large amounts of straw were decomposed on the surface for up to 18 days; after 54 days it had no effect on germination. Immobilization of nitrogen occurred mainly when the straw was mixed with the soil, or when surface-rotted straw was ploughed into the soil just before seeding. The latter effect could not be overcome by the addition of mineral nitrogen. Part II, Plant and Soil 38, 347–361 (1973).     

油菜秸秆还田对水稻根系、分蘖和产量的影响

采用田间试验与栽培模拟试验相结合的方法,分析了油菜秸秆还田对水稻根系、分蘖和产量的影响.结果表明: 水稻移栽后0～36 d,与秸秆不还田处理相比,油菜秸秆还田处理下水稻分蘖减少1～2个,根系单株伤流量降低1.0～8.6 mg,根系谷氨酰胺合成酶(GS)、谷丙转氨酶(GPT)和谷草转氨酶(GOT) 活性分别降低0.10～6.11、0.06～0.31和0.52～0.84 μmol·g^-1·h^-1. 水稻移栽后56 d,与秸秆不还田处理相比,油菜秸秆翻埋还田处理下水稻根系单株伤流量增加3.4～11.7 mg,根系GS、GPT和GOT活性分别增加0.34～0.78、0.13～0.45和0.18～0.20 μmol·g^-1·h^-1;油菜秸秆覆盖还田处理下水稻根系单株伤流量降低19～25 mg,根系GS、GPT和GOT活性分别增加0.16～0.34、0.08～0.21和0.06～0.32 μmol·g^-1·h^-1.油菜秸秆还田处理中,全量还田处理下的水稻产量最高,其中,与全量覆盖还田相比,全量翻埋还田处理下的水稻产量增加0.13～0.48 t·hm^-2.可见,油菜秸秆还田会导致水稻生长前期根系活力下降、氮代谢酶活性降低,从而使水稻根系生长缓慢、返青延迟,但在中后期,随着根系活力和氮代谢酶活性的增强,秸秆还田会促进水稻根系生长;油菜秸秆还田对水稻产量的影响是多因素综合作用的结果,全量翻埋还田更适宜于四川油稻两熟轮作系统.     

油菜秸秆还田对水稻根系、分蘖和产量的影响

采用田间试验与栽培模拟试验相结合的方法,分析了油菜秸秆还田对水稻根系、分蘖和产量的影响.结果表明: 水稻移栽后0～36 d,与秸秆不还田处理相比,油菜秸秆还田处理下水稻分蘖减少1～2个,根系单株伤流量降低1.0～8.6 mg,根系谷氨酰胺合成酶(GS)、谷丙转氨酶(GPT)和谷草转氨酶(GOT) 活性分别降低0.10～6.11、0.06～0.31和0.52～0.84 μmol·g^-1·h^-1. 水稻移栽后56 d,与秸秆不还田处理相比,油菜秸秆翻埋还田处理下水稻根系单株伤流量增加3.4～11.7 mg,根系GS、GPT和GOT活性分别增加0.34～0.78、0.13～0.45和0.18～0.20 μmol·g^-1·h^-1;油菜秸秆覆盖还田处理下水稻根系单株伤流量降低19～25 mg,根系GS、GPT和GOT活性分别增加0.16～0.34、0.08～0.21和0.06～0.32 μmol·g^-1·h^-1.油菜秸秆还田处理中,全量还田处理下的水稻产量最高,其中,与全量覆盖还田相比,全量翻埋还田处理下的水稻产量增加0.13～0.48 t·hm^-2.可见,油菜秸秆还田会导致水稻生长前期根系活力下降、氮代谢酶活性降低,从而使水稻根系生长缓慢、返青延迟,但在中后期,随着根系活力和氮代谢酶活性的增强,秸秆还田会促进水稻根系生长;油菜秸秆还田对水稻产量的影响是多因素综合作用的结果,全量翻埋还田更适宜于四川油稻两熟轮作系统.     

土壤有机碳和微生物群落结构对多年不同耕作方式与秸秆还田的响应

土壤有机碳对维持陆地生态系统功能和缓解土壤退化问题至关重要,土壤微生物参与土壤有机碳的循环过程,而耕作方式与秸秆还田影响土壤有机碳和微生物群落.本试验采用裂区试验设计,耕作方式为主区,分别设深松(ST)和旋耕(RT)处理,副区为秸秆还田量,分别设秸秆全还田(F)和秸秆不还田(0)处理,采用Illumina测序技术测定土壤微生物群落结构和固碳功能基因,并测定了2012—2017试验年间土壤有机碳含量.结果表明: 1)深松耕作和秸秆还田均显著提高了pH、微生物生物量碳、总氮、粉粒含量、黏粒含量,而显著降低了砂粒含量; 2)试验年间各处理的土壤有机碳(SOC)含量均呈增加趋势,但与旋耕耕作和秸秆不还田处理相比,深松耕作和秸秆还田处理的平均有机碳增量分别显著提高30.6%和33.2%; 3)土壤中最丰富的细菌类型为变形菌门,其次为酸杆菌门和芽单胞菌门; 4)深松秸秆还田处理(STF)具有较高的微生物多样性; 5)除砂粒含量外,土壤pH、微生物生物量碳、总氮、粉粒和黏粒含量均促使深松秸秆全还田处理下的微生物群落结构向着有利于有机碳积累的方向发生变异; 6)除二糖和寡糖代谢途径外,CO₂固定、发酵、主要碳水化合物代谢、一碳代谢、糖醇、有机酸、糖苷水解酶类的代谢功能基因丰度均表现为深松耕作显著高于旋耕,且均与土壤有机碳呈正相关关系.因此,深松结合秸秆还田能够改善土壤基本性质与土壤微生物群落结构,有利于增加土壤固碳能力和解决土壤退化问题.     

Nitrate-dependent iron(II) oxidation in paddy soil

Iron(III) profiles of flooded paddy soil incubated in the greenhouse indicated oxidation of iron(II) in the upper 6 mm soil layer. Measurement of oxygen with a Clark-type microelectrode showed that oxygen was only responsible for the oxidation of iron(II) in the upper 3 mm. In the soil beneath, nitrate could be used as electron acceptor instead of oxygen for the oxidation of the iron(II). Nitrate was still available 3 mm below the soil surface, and denitrifying activity was indicated by higher concentrations of nitrite between 3 and 6 mm soil depth. Nitrate was generated by nitrification from ammonium. Ammonium concentrations increased beneath 6 mm soil depth, indicating ammonium release and diffusion from deeper soil layers. High concentrations of ammonium were also found at the surface, probably resulting from N2 fixation by cyanobacteria. Experimental adjustment of the nitrate concentration in the flooding water to 200 microM stimulated nitrate-dependent iron(II) oxidation, which was indicated by significantly lower iron(II) concentrations in soil layers in which nitrate-dependent iron(II) oxidation was proposed. Soil incubated in the dark showed high iron(III) concentrations only in the layer where oxygen was still available. In this soil, the nitrogen pool was depleted because of the lack of N2 fixation by cyanobacteria. In contrast, soil incubated in the dark with 500 microM nitrate in the flooding water showed significantly higher iron(II) and significantly lower iron(II) concentrations in the anoxic soil layers, indicating nitrate-dependent iron(II) oxidation. Anoxic incubations of soil with nitrate in the flooding water also showed high concentrations of iron(II) and low concentrations of iron(II) in the upper 3 mm. As oxygen was excluded in anoxic incubations, the high iron(III) concentrations are a sign of the activity of nitrate-dependent iron(II) oxidizers. The presence of these bacteria in non-amended soil was also indicated by the most probable number (MPN) counts of nitrate-dependent iron(II) oxidizers in the layer of 3-4 mm soil depth, which revealed 1.6 x 10(6) bacteria g(-1) dry weight.     

A greenhouse study on the effect of inoculation of N-fixing blue-green algae in an alluvial soil treated with P and Mo on the yield of rice and changes in the N-content of soil

Summary The efficiency of the inoculation of three cultures of N-fixing blue-green algaeviz. (i)Aulosira fertilissima (A₁), (ii)Nostoc muscorum (A₂) and (iii) their mixture (A₃) in increasing the grain and straw yield of rice, nitrogen uptake in grain and nitrogen content in soil was studied in a green house experiment with an alluvial soil in presence or absence of urea nitrogen application. Inoculation significantly increased the grain and straw yield of rice and nitrogen uptake in grain, but the efficiency of inoculation gradually decreased with the increase in the levels of urea nitrogen application, the extent of decrease varying with the algal cultures inoculated. The nitrogen content in the soils after the crop harvest recorded a significant increase due to inoculation but after air drying the soil a marker decrease of the same was observed, which indicated that most of the nitrogen added to the soil by blue-green algae through fixation did not persist after air drying the soil.     

秸秆还田下施氮量对稻茬晚播小麦土壤氮素盈亏的影响

在大田条件下,研究了不同施氮量对秸秆还田下晚播小麦土壤矿质氮含量变化、秸秆氮释放及小麦产量的影响.结果表明： 0～50 cm土层土壤矿质氮含量随着施氮量的增加而显著增加,随生育进程的推进,N₂₇₀和N₃₆₀处理下层土壤的矿质氮显著积累.秸秆氮素释放量随施氮量增加而增加,越冬至拔节期氮释放量最低,拔节至成熟期释放量占总释氮量的50%以上.全生育期施氮量超过180 kg·hm^-2,土壤氮素开始出现显著的盈余,播种至拔节期氮素表观盈余量显著高于拔节至成熟期.籽粒产量在270 kg·hm^-2施氮量下最高, 更高施氮量下氮素利用效率显著降低.施氮量为270 kg·hm^-2时,有利于秸秆全量还田下晚播小麦兼顾产量和生态效益.     

Soybean genotypic differences in sensitivity of symbiotic nitrogen fixation to soil dehydration

Nitrogen fixation activity by soybean (Glycine max (L.) Merr.) nodules has been shown to be especially sensitive to soil dehydration. Specifically, nitrogen fixation rates have been found to decrease in response to soil dehydration preceding alterations in plant gas exchange rates. The objective of this research was to investigate possible genetic variation in the sensitivity of soybean cultivars for nitrogen fixation rates in response to soil drying. Field tests showed substantial variation among cultivars with Jackson and CNS showing the least sensitivity in nitrogen accumulation to soil drying. Glasshouse experiments confirmed a large divergence among cultivars in the nitrogen fixation response to drought. Nitrogen fixation in Jackson was again found to be tolerant of soil drying, but the other five cultivars tested, including CNS, were found to be intolerant. Experiments with CNS which induced localized soil drying around the nodules did not result in decreases in nitrogen fixation rates, but rather nitrogen fixation responded to drying of the entire rooting volume. The osmotic potential of nodules was found to decrease markedly upon soil drying. However, the decrease in nodule osmotic potential occurred after significant decreases in nitrogen fixation rates had already been observed. Overall, the results of this study indicate that important genetic variations for sensitivity of nitrogen fixation to soil drying exist in soybean, and that the variation may be useful in physiology and breeding studies.     

Nitrogen availability to Pseudomonas fluorescens DF57 is limited during decomposition of barley straw in bulk soil and in the barley rhizosphere.

The availability of nitrogen to Pseudomonas fluorescens DF57 during straw degradation in bulk soil and in barley rhizosphere was studied by introducing a bioluminescent reporter strain (DF57-N3), responding to nitrogen limitation, to model systems of varying complexity. DF57-N3 was apparently not nitrogen limited in the natural and sterilized bulk soil used for these experiments. The soil was subsequently amended with barley straw, representing a plant residue with a high carbon-to-nitrogen ratio (between 60 and 100). In these systems the DF57-N3 population gradually developed a nitrogen limitation response during the first week of straw decomposition, but exclusively in the presence of the indigenous microbial population. This probably reflects the restricted ability of DF57 to degrade plant polymers by hydrolytic enzymes. The impact of the indigenous population on nitrogen availability to DF57-N3 was mimicked by the cellulolytic organism Trichoderma harzianum Rifai strain T3 when coinoculated with DF57-N3 in sterilized, straw-amended soil. Limitation occurred concomitantly with fungal cellulase production, pointing to the significance of hydrolytic activity for the mobilization of straw carbon sources, thereby increasing the nitrogen demand. Enhanced survival of DF57-N3 in natural soil after straw amendment further indicated that DF57 was cross-fed with carbon/energy sources. The natural barley rhizosphere was experienced by DF57-N3 as an environment with restricted nitrogen availability regardless of straw amendment. In the rhizosphere of plants grown in sterilized soil, nitrogen limitation was less severe, pointing to competition with indigenous microorganisms as an important determinant of the nitrogen status for DF57-N3 in this environment. Hence, these studies have demonstrated that nitrogen availability and gene expression in Pseudomonas is intimately linked to the structure and function of the microbial community. Further, it was demonstrated that the activities of cellulolytic microorganisms may affect the availability of energy and specific nutrients to a group of organisms deficient in hydrolytic enzyme activities.     

秸秆预处理对土壤微生物量及呼吸活性的影响

冬小麦秸秆经8．0g·L^-1H2O2(pH11．0)溶液、12．5g·L^-1 NaOH溶液或H2SO4溶液浸泡8h并80℃烘干后,与无机N一起加入土壤,进行室内25℃恒温培养试验,在不同时间测定土壤微生物量C、N和CO2释放速率。结果表明,培养前期,秸秆预处理使土壤微生物量C数量增加了1．0～1．4倍,但降低了土壤微生物的呼吸活性;培养后期,NaOH和H2SO4处理使土壤微生物量C分别下降了28％和42％,但增加了土壤微生物的呼吸活性;H2O2处理则使土壤微生物量N增加90％;土壤微生物区系中的真菌比例在不同时刻有所增加,表明将秸秆预处理后施入土壤,将对土壤中微生物数量和呼吸活性产生一定影响。