利用上流式双层厌氧滤器启动厌氧氨氧化研究

厌氧氨氧化是一种高效的脱氮处理工艺,但其启动和运行过程困难,高效反应器是解决此问题的有效手段。本文利用改进的上流式双层厌氧滤器开展厌氧氨氧化启动反应的试验研究。在反应器填料上分别接种反硝化污泥、厌氧污泥、混合污泥,通过模拟废水提供自养反硝化条件,并逐步提高基质浓度和水力负荷,促使菌群向厌氧氨氧化反应转变。试验发现,反硝化污泥、厌氧污泥、混合污泥均可启动厌氧氨氧化反应,启动时间分别为42、54 d和45 d。以反硝化污泥为接种物的启动效果最好,启动时间较短且废水氮素去除率高,总氮去除率最高达到82.2%。双层填料的反应器有效提高了厌氧氨氧化的稳定性,该反应器中厌氧氨氧化菌对氨氮、亚硝氮的适宜浓度负荷为270、360 mg·L~(-1),废水中COD浓度不宜超过150 mg·L~(-1),系统中存在厌氧氨氧化和甲烷化共存的效应。     

包埋法固定光合细菌技术对光合产氢能力的影响

研究了不同包埋材料的包埋法固定化光合细菌的产氢能力,结果表明琼脂、海藻酸钠、PVA.硼酸固定光合菌体对光合细菌的产氢量、产氢速率、比产氢速率都有不同程度的提高,海藻酸钠固定化光合菌体对产氢最为有利,比游离态产氢量提高15%～40%,平均产氢速率是游离态产氢速率的1.37倍;琼脂次之,比游离态产氢量提高8%～15%;PVA-硼酸包埋光合细菌产氢能力在前3天内有较好的效果,但随着时间的延长反而不及游离态状态下产氢,72 h以内的产氢量比游离态产氢量提高10%～20%.聚丙烯酰胺包埋光合细菌的产氢量还不到游离态产氢量的60%,所以聚丙烯酰胺不适宜作为光合细菌产氢时的包埋材料.     

提高猪场沼液净化处理效果的氨吹脱控制参数

针对畜禽养殖场沼气工程沼液氨氮浓度高,碳氮比不足,直接采用传统生化污水处理法效果不佳的问题,该文对氨吹脱工艺降低猪场沼液氨氮浓度参数进行了试验研究,探索了不同初始氨氮浓度、pH值、气液比、温度等参数对氨氮去除的效果,并进一步研究了Ca(OH)2的混凝作用。结果表明:初始氨氮质量浓度分别为500和900mg/L时,氨氮去除率无显著差异。在初始氨氮质量浓度为900mg/L,pH值为10.5,气液比(流量比)2000,沼液温度30℃的运行条件下,氨氮去除率较高为81.84%。在Ca(OH)2投加量为5.0g/L条件下,混凝沉淀效果较好,化学需氧量(COD)、总磷(TP)和PO43-去除率分别为30.13%、97.44%和98.76%,但总硬度提高了106%。该文研究结果为开发沼液深度处理工艺提供了数据。     

长期定位施肥对中性紫色土硝化作用及氨氧化微生物的影响

为了研究长期不同施肥措施对中性紫色土氨氧化微生物及其硝化作用的影响,以国家紫色土肥力与肥料效益监测基地的中性紫色土为研究对象,进行土壤氨氧化细菌和氨氧化古菌amo A基因的Real-time PCR分析,比较长期不同定位施肥对土壤氨氧化潜势和硝化强度的影响,并分析不同施肥制度对功能微生物丰度与功能的作用。数据显示,土壤中氨氧化古菌amo A基因拷贝数(Log值6.21～7.14)远大于氨氧化细菌(Log值3.65～5.73),相对于对氨氧化细菌丰度的影响,施肥对土壤氨氧化古菌丰度影响较小。施用氮肥与磷肥都显著提高了土壤氨氧化细菌丰度,1.5NPK+M处理氨氧化细菌丰度最高(Log值5.73),有机无机肥配施可以显著提高土壤氨氧化微生物丰度;而含氯化肥的施用在一定程度上降低了土壤氨氧化细菌丰度与硝化细菌生长,与施用不含氯的肥料处理相比,含氯肥料处理的土壤氨氧化细菌丰度与硝化细菌数分别降低了3.74%和88.12%。研究表明,长期施肥能影响中性紫色土中氨氧化细菌的丰度,有机无机肥配施能够提高土壤的氨氧化潜力与土壤的硝化能力。     

添加生物炭改善菜地土壤氨氧化细菌群落并提高净硝化率

  【目的】  氨氧化过程是硝化作用的限速步骤，对氮循环有着重要影响。本研究通过分析生物炭输入下土壤氨氧化微生物群落的变化，揭示其影响土壤硝化作用的生物学机制。  【方法】  以华北潮土区设施菜地土壤为对象，设置生物炭梯度 (C₀、C_0.5、C_1.5、C_4.0) 土壤培养试验，结合PCR和T-RFLP等分析技术，观测生物炭输入下土壤氨氧化细菌群落变化动态，解析生物炭、土壤硝化作用与氨氧化细菌群落之间的关系。  【结果】  添加生物炭明显改变了土壤氨氧化微生物群落结构及氮素硝化过程。与未添加生物炭处理相比，生物炭添加处理培养前期土壤氨氧化细菌群落Shannon、Evenness指数分别升高5.4%～18.8%、26.2%～33.8%，后期Shannon指数降低20.7%～34.2%。生物炭输入对AOA群落没有明显影响，AOB群落256、58 bp代表物种丰度分别增加61.4%～56.0%、60.6%～78.6%，488 bp代表物种丰度降低22.8%～26.9%。21 bp代表物种丰度前期增加后期降低，与491 bp代表物种丰度变化相反。添加生物炭土壤AOB amoA基因丰度增加48.9%～53.2%。土壤NO₃–-N含量提高1.7%～25.6%，NH₄+-N含量下降13.4%～31.1%，土壤净硝化速率提高21.8%～70.2%。  【结论】  生物炭的输入可以改善以AOB为主的土壤氨氧化微生物群落结构，提高amoA酶活性，但是对氨氧化古菌微生物群落结构未产生明显影响。因此，生物炭提高土壤净硝化速率的作用与其对土壤氨氧化细菌群落和组成的影响密切相关。     

尿素和生物炭施用对菜地土壤氨氧化作用的影响

研究将生物炭(40000 kg hm~(-2))和不同用量的尿素(0, 150, 300, 450 kg hm~(-2))施用于酸性红壤中,连续种植四季作物后采集菜地土壤样品,通过定量PCR方法测定添加硝化抑制剂后土壤氨氧化微生物数量和土壤氨氧化潜势的变化,并分析氨氧化古菌(AOA)和氨氧化细菌(AOB)对土壤氨氧化潜势的相对贡献,深入探讨生物炭和氮肥添加对菜地土壤氨氧化微生物和氨氧化潜势的影响。结果表明,与未添加生物炭相比,添加生物炭处理土壤容重降低了7.1%～11.5%,pH值提高了0.20～0.56个单位,有机质含量增加了13.5%～19.1%;与未施氮肥处理相比,无机氮的含量增加了38.5%～77.8%(未添加生物炭)和17.1%～59.5%(添加生物炭)。添加生物炭和氮肥处理AOA的基因拷贝数没有显著差异(P 0.05),氮肥添加提高了AOB的基因拷贝数147.5%～385.6%(未添加生物炭)和69.5%～514.0%(添加生物炭)。添加生物炭处理,随氮肥施用量的增加,氨氧化潜势降低了13.4%～20.7%。因此,本研究中氮肥添加使AOB的amoA基因拷贝数显著增加、氨氧化潜势显著下降,对AOA没有显著影响(P 0.05);AOA对氨氧化潜势起到了主导作用;生物炭和尿素添加通过改变土壤的无机氮含量、pH、有机质含量影响土壤氨氧化过程。     

基于CaO调节的太阳能辅助加热猪粪沼液氨吹脱工艺研究

氨吹脱工艺可在氨氮高效去除的同时实现氮素转化，是沼液养分回收的理想方案。在传统吹脱工艺中，碱剂添加，特别是NaOH和加热成本占总成本70%以上，导致运行成本较高。为降低猪粪沼液氨吹脱工艺能耗，该研究探讨使用低成本钙剂CaO替代NaOH调节沼液pH值，采用太阳能加热替代传统加热耦合氨吹脱工艺处理沼液。结果表明：CaO不仅能调节沼液pH值，还具有一定絮凝效果，且以石灰乳形态添加效果更好。当添加浓度为5 g/L时，沼液pH值不低于12.0，沼液浊度、COD、TP去除率分别为88.1%、50.1%、93.8%。不同吹脱组（氨氮去除率高于80%）运行成本结果表明，氨吹脱工艺在高pH值（12.0）驱动而不加热（25 ℃）时沼液处理成本最低，为2.46元/m³，与温度驱动相比，成本降低了52.1%～68.7%。而加热可进一步提升氨氮去除率，将太阳能加热与氨吹脱工艺耦合实现了氨氮去除率的显著提升，沼液经10%石灰乳形态CaO以添加浓度为5 g/L调节后，利用自制的太阳能辅助加热的氨吹脱装置在夏季可获得超过97.5 %的氨氮去除率，即使在冬季氨氮去除率也超过86%。该研究结果可为太阳能耦合氨吹脱低成本氨氮去除工艺实际应用提供可行性依据。     

固定化水华束丝藻和硅藻土对畜禽废水COD净化分析

利用海藻酸钠-聚乙烯醇凝胶固定化水华束丝藻和硅藻土,研究不同包埋比例(即m湿藻∶m硅藻土)对COD的净化效果,随着包埋比的增加,包埋粒对水体中COD的去除能力呈先增加后降低的趋势。当包埋比为1∶4时,净化效果最好,对COD的去除率为86.34%。     

固态抑氨菌剂制备及其对蛋鸡舍的抑氨效果

为了为抑氨菌选择良好的固定化载体,并研究固态抑氨菌剂对降低鸡舍内氨质量浓度的效果,该文将7种有机载体混合成63种组合载体后,选择较佳的组合载体,并以此制成固态抑氨菌剂。于饲喂1000只商品蛋鸡的笼养蛋鸡舍中,将固态抑氨菌剂均匀撒放于鸡粪表面,研究其在鸡舍现场的抑氨效果。菌剂的撒放按照菌剂与鸡粪质量之比进行,试验1期为0.5%,试验2期为1%,试验3期为1.5%,对照1期、2期和3期均不撒放,每天4次测定鸡舍内6个点的温度、相对湿度、氨质量浓度和CO2体积分数,试验共进行36d。结果表明,麦糠、稻壳和玉米芯粉等量混合并以200%吸水率吸附抑氨菌液后制成的固态抑氨菌剂的效果较佳;试验1期鸡舍内氨质量浓度未发生显著变化(P>0.05),试验2期氨质量浓度降低15%(P<0.01),试验3期氨质量浓度降低59.3%(P<0.01);但3期试验均未对舍内CO2体积分数产生显著影响(P>0.05)。结果显示,以有机混合载体吸附抑氨菌液制成的固态抑氨菌剂有明显降低笼养蛋鸡舍内氨质量浓度的作用。该研究结果为生产过程中有效控制蛋鸡舍内的氨质量浓度提供理论参考。     

桂西北不同植被恢复阶段土壤氨氧化细菌遗传多样性研究

以桂西北喀斯特不同植被恢复阶段(草丛、灌木林、次生林、原生林)生态系统为研究对象,运用分子生物学技术分析了土壤氨氧化细菌amoA功能基因多样性,探讨了其与脲酶活性和土壤理化性质的关系.结果显示,随着植被的恢复,土壤氨氧化细菌多样性指数与均匀度指数呈增大趋势(灌木林例外),且土壤中氨氧化细菌群落结构发生了改变:主要表现在因Nitrosospira3簇种群对铵态氮浓度敏感度差异导致其在3a、3b簇中分布不一致;相关分析表明;土壤脲酶活性与铵态氮浓度呈正相关关系,土壤脲酶可能通过影响铵态氮浓度改变氨氧化细菌多样性,但植被恢复后期土壤铵态氮浓度减少并未降低土壤氨氧化细菌多样性.LIBSHUFF和RDA分析揭示,植被类型和土壤脲酶活性及pH与氨氧化细菌群落结构紧密相关,说明植被和土壤氮素有效性以及pH可能是决定土壤氨氧化细菌多样性的主要因子,为深入理解喀斯特地区土壤氮素循环提供了一定的科学依据.     

海藻酸钠固定化细菌对毒死蜱的降解特性

毒死蜱的生产和使用日趋广泛,由其造成的环境污染和危害不容忽视。微生物是影响有机磷农药在环境中降解的最主要因素,也被认为是降解有机磷农药最可靠而高效的途径。固定化技术是提高微生物降解农药效率的有效方法之一。本研究以海藻酸钠为载体,采用注射器滴定法将蜡状芽孢杆菌(Bacillus cer-eus)HY-1用海藻酸钠溶胶包埋,研究了反应时间、固定化菌接入量、pH和毒死蜱初始浓度对毒死蜱降解的影响以及固定化菌的重复使用效果。结果表明:海藻酸钠固定化菌能够高效降解基础培养基中的毒死蜱,制备固定化小球海藻酸钠溶胶的最适浓度为2.5%(w/v),小球的平均粒径为3 mm。在培养时间为60 h时,固定化菌对100 mg·L-1毒死蜱的降解率达到最大。固定化小球接入量为160 g·L-1时,对100 mg·L-1毒死蜱的降解率最高。固定化菌对毒死蜱的降解有着较宽泛的pH适应范围,碱性环境更有利于其对毒死蜱的有效降解。当毒死蜱初始浓度为80 mg·L-1和100 mg·L-1时,固定化菌对毒死蜱的降解率较高,达90%左右。固定化菌可重复利用降解毒死蜱,当利用4次后,固定化小球虽已发生崩解,但对100 mg·L-1毒死蜱的降解率仍高达47%。因此,海藻酸钠固定化蜡状芽孢杆菌对水体中毒死蜱的降解率较高,环境适应性较强,固定化菌可在毒死蜱污染的净化去毒方面发挥重要作用。     

Immobilization and mineralization of nitrogen in soils incubated with pig slurry or ammonium sulphate

Nitrogen mineralization and immobilization were investigated in two soils incubated with ammonium sulphate or pig slurry over a range of temperatures and moisture contents. A reduction in the mineralization of soil organic N was observed in soils incubated with 100 μg NH₄⁺-Ng^?1 soil as ammonium sulphate at 30°C but not at lower temperatures. Addition of 100 μg NH₄⁺-N g^?1 soil as pig slurry resulted in a period of nett immobilization lasting up to 30 days at 5°C. Although the length of the immobilization phase was shorter at higher temperatures the total N immobilized was similar. The subsequent rate of mineralization in slurry-treated soils was not significantly greater (P = 0.05) than in untreated soils. There was no evidence of any subsequent increased mineralization arising from the immobilized N or slurry organic N for up to 175 days. The rate of immobilization was found to increase with increasing moisture content, though the period of nett immobilization was shorter, so that the amount of N immobilized was similar over a range of moisture contents from 10 to 40%. Approximately 40% of the NH₄⁺-N in the slurry was immobilized under the incubation conditions used.     

Characterization and extract ability of immobilized 15N from the soil microbial biomass

The microbial biomass of a typical Illinois Mollisol (Flanagan silt loam) was labeled with ¹⁵N, and several extradants were tested to determine their effectiveness in separating the immobilized ¹⁵N from the native soil N. From 3 to 5% of the total N and from 7 to 11% of the tracer N were removed by the milder extradants (i.e. hot water, hot 10mM CaCl₂, hot 5mm NaHCO₃, and cold 10mm NaHCO₃). Acidified permanganate (0.1 m KMnO₄ in 2 m H₂SO₄) and anhydrous formic acid were the most intensive extradants tested; they removed from 10 to 13% of the total N and about 14% of the immobilized ¹⁵N. An inverse relationship was observed between the amount of N extracted and selectivity of the extradants for removing the microbial ¹⁵N, indicating that the milder procedures were more selective in extracting the immobilized ¹⁵N.Distinct differences in the chemical distribution of organic N were observed for the immobilized ¹⁵N and native soil N. Lower proportions of the immobilized ¹⁵N were accounted for as acid-insoluble N and ammonia N (NH₃-N); while higher proportions were found in the amino acid and hydrolyzable unknown (HUN) N fractions.     

Effects of glucose and rhizodeposits (with or without cysteine-S) on immobilized-35S, microbial biomass-35S and arylsulphatase activity in a calcareous and an acid brown soil

Our aim was to study the effects of C (as glucose and artificial rhizodeposits) on S immobilization, in relation to microbial biomass‐S and soil arylsulphatase (ARS) activity, in contrasting soils (a calcareous and an acid brown soil). The glucose‐C and artificial rhizodeposit‐C with or without cysteine were added at six rates (0, 100, 200, 400, 600 and 800 mg kg^?1 soil) to the two soils and then incubated with Na₂³⁵SO₄ for 1 week prior to analysis. The percentages of ³⁵S immobilized increased when C as glucose and rhizodeposit (without cysteine) were added to both soils. With cysteine‐containing rhizodeposit, the percentages of ³⁵S immobilized remained relatively stable (23.5% to 29.9%) in the calcareous soil, but decreased in the acid brown soil (52.7% to 31.5%). For both soils, cysteine‐containing rhizodeposit additions showed no significant correlation between immobilized‐³⁵S and microbial biomass‐³⁵S, suggesting that microorganisms immobilized cysteine‐S preferentially instead of ³⁵S from the tracer (Na₂³⁵SO₄). In the calcareous soil, a positive and significant correlation was found between ARS activity and microbial biomass‐³⁵S (r = 0.85, P < 0.05) when glucose was added. We also saw this correlation in the acid brown soil when rhizodeposit‐C without cysteine was added (r = 0.90, P < 0.05). Accordingly, the results showed the presence of extracellular arylsulphatase activity of 48.7 mg p‐nitrophenol kg^?1 soil hour^?1 in the calcareous soil and of 27.0 mg p‐nitrophenol kg^?1 soil hour^?1 in the acid brown soil.     

Effect of microbial nitrogen immobilization during the growth period on the availability of nitrogen fertilizer for winter cereals

 Pot and field experiments were conducted to determine microbial immobilization of N fertilizer during growth periods of winter wheat and winter barley. In a pot experiment with winter wheat, Ca(¹⁵NO₃)₂ was applied at tillering [Zadok's growth stage (GS) 25)], stem elongation (GS 31) and ear emergence (GS 49). Rates of 100 mg N pot^–1, 200 mg N pot^–1 or 300 mg N pot^–1 were applied at each N application date. At crop maturity, ¹⁵N-labelled fertilizer N immobilization was highest at the highest N rate (3×300 mg N pot^–1). For each N-rate treatment about 50% of the total immobilized fertilizer N was immobilized from the first N dressing, and 30% and 20% of the total ¹⁵N immobilized was derived from the second and third applications, respectively. In field trials with winter wheat (three sites) and winter barley (one site) N was applied at the same growth stages as for the pot trial. N was also applied to fallow plots, but only at GS 25. N which was not recovered (neither in crops nor in soil mineral N pools) was considered to represent net immobilized N. A clear effect of N rate (51–255 kg N ha^–1) on net N immobilization was not found. The highest net N immobilization was found for the period between GS 25 (March) and GS 31 (late April) which amounted to 54–97% of the total net N immobilized at harvest (July/August). At GS 31, non-recovered N was found to be of similar magnitude for cropped and fallow plots, indicating that C from roots did not affect net N immobilization. Microbial biomass N (N_mic) was determined for cropped plots at GS 31. Although N_mic tended to be higher in fertilized than in unfertilized plots, fertilizer-induced increases in N_mic and net N immobilization were poorly correlated. It can be concluded that microbial immobilization of fertilizer N is particularly high after the first N application when crop growth and N uptake are low. Received: 6 July 1999     

Immobilization of Carbonic Anhydrase on Chitosan Stabilized Iron Nanoparticles for the Carbonation Reaction

Carbonic anhydrase (CA) has been immobilized on chitosan stabilized iron nanoparticles (CSIN) for the biomimetic carbonation reaction. CSIN was characterized using scanning electron microscope, energy dispersive X-ray, X-ray diffraction spectroscopy, and Fourier transform infrared analysis. The effect of various parameters such as pH, temperature and storage stability, on immobilized CA was investigated using a p-NPA assay. Kinetic parameters of immobilized and free CA (K _m and V _max values) were also evaluated. The K _m and V _max for immobilized CA was 1.727?mM and 1.189???mol?min^?1?ml^?1, respectively, whereas for free enzyme the K _m and V _max was 1.594?mM and 1.307???mol?min^?1?ml^?1, respectively. It was observed that the immobilized enzyme had longer storage stability and retained 50?% of its initial activity upto 30?days at room temperature. CA immobilized on CSIN has been used for hydration of CO₂, and the results were validated by using a gas chromatographic method. Proof of concept has been established for the biomimetic carbonation reaction. Immobilized CA show reasonably good CO₂ sequestration capacity of 21.55?mg of CaCO₃/mg of CA as compared to CO₂ sequestration capacity of 34.92?mg of CaCO₃/mg of CA for free CA respectively, under a limiting concentration of CO₂ (14.5?mg of CO₂/10?ml).     

The Oxidation of Di-(2-Ethylhexyl) Phthalate (DEHP) in Aqueous Solution by UV/H2O2 Photolysis

The oxidation of di-(2-ethylhexyl) phthalate (DEHP) in solution using UV/H₂O₂ and direct UV photolysis are analyzed in this study. It was found that DEHP was 100% removal in the solution by 180-min UV/H₂O₂ treatment and 73.5% removal by 180-min direct UV photolysis. The effect of different factors, such as DEHP concentration, H₂O₂ concentration, and UV light intensity, on photochemical degradation was investigated. The degradation mechanism of DEHP and the acute toxicity of intermediates were also studied. The photochemical degradation process was found to follow pseudo-first-order kinetics. The results of our study suggested that the concentration with 40 mg/L H₂O₂ and 5 μg/mL DEHP in the solution at pH 7 with 10.0?×?10^?6 Einstein l^?1?s^?1 UV was the optimal condition for the photochemical degradation of DEHP. The photochemical degradation with UV/H₂O₂ can be an efficient method to remove DEHP in wastewater.     

通过土壤泥浆中的过氧化氢处理三氯乙烯污染的土壤

Chlordecone, one of the most persistent organochlorine pesticides, was applied between 1972 and 1993 in banana fields in the French West Indies, which results in long-term pollution of soils and contamination of waters, aquatic biota, and crops. As human exposure to chlordecone is mainly due to food contamination, early research was focused on chlordecone transfer to crops. Field trials were conducted to investigate chlordecone contamination of yam, sweet potato, turnip, and radish grown on a ferralic Nitisol polluted by chlordecone. We also carried out trials on yam, courgette, and tomato under greenhouse conditions with homogenized Andosol and Nitisol, polluted by chlordecone to various extents. Our results indicated that i) all tubers were contaminated in accordance with the chlordecone content of the soils; ii) the contamination capacity of the Nitisol was greater than that of the Andosol; and iii) whatever the soil type, tuber contamination was related to the soil volumetric content of dissolved chlordecone. Nevertheless, no tubers showed sufficient chlordecone uptake for efficient soil decontamination by means of plant extraction. Soil contact accounted for most of the root crop contamination, which was inversely proportional to the tuber size. Internal transfer might also increase root crop contamination when the root central cylinder contained raw sap flow, as in the case of turnip or radish. Courgette fruits showed high contamination without soil contact. Thus, further research is needed to explore the pattern of both below- and aboveground plant chlordecone contamination and assess the hypothesis of its correlation with sap flow. Finally, we used our results to build a decision-making tool for farmers, relating soil pollution with the maximal contamination of the harvested organs to predict crop contamination and thus assisting farmers in making crop choices at planting in order to conform with the European Union’s regulations.     

一株耐盐苯酚降解酵母菌的分离及降解特性研究

从化工厂污泥中分离到一株酵母菌 ,初步鉴定为德氏酵母属 (Debaryomycessp ) ,命名为Gb。该菌株可以在 0～ 2 0 %Na2 SO4环境中生长 ,并能以苯酚为唯一碳源和能源。其苯酚降解最适浓度为 1 0 0 0mgL-1 ,最适Na2 SO4浓度为 5 %,最适pH和温度分别为 5 5和 30℃ ,在 2 5 0ml三角瓶中最适装液量为 1 0 0ml。当Na2 SO4盐浓度为 5 %、苯酚浓度为 1 0 0 0mgL-1 时 ,最适条件下培养 3天即能降解 95 %的苯酚。本文还对其耐盐机理进行了初步研究 ,发现细胞内海藻糖含量随外界盐浓度增加而增加 ,表明Debaryomycessp 在高盐条件下能以海藻糖作为渗透调节物质。     

Utilization of organic materials in soil aggregates by bacteria and fungi

Cultures of six fungi and two bacteria were added to samples of aggregates in which either ¹⁴C-labelled glucose or starch was thoroughly distributed in macro- and micropores or in control samples where the labelled substrates were added to the preformed aggregates and considered to be mainly in macropores. The release of ¹⁴CO₂ was monitored over a 24-day incubation.In the control samples with substrates mainly in macropores, the bacteria were as active as fungi in releasing ¹⁴CO₂ from both soils. When the substrates were distributed in macro- and micropores in aggregates made from a fine sandy loam, the fungi were more efficient than bacteria in releasing ¹⁴CO₂. This was not the case in a self-mulching clay.The initial flush of ¹⁴CO₂ released during incubation of the amended fine sandy loam was due mainly to fungi, which were followed by a secondary bacterial population. The change in populations occurred simultaneously with a step in the cumulative ¹⁴CO₂ release curve thought to be due to the utilization of all the labelled substrate added, followed by renewed respiration as the secondary population flourished. The results presented fit well with an efficiency of C assimilation by micro-organism in soil of about 60%.