基于NH_2-MIL-101(Fe)过氧化物模拟酶特性测定葡萄糖          下载免费PDF全文

万路  黄玉明  奉萍 《西南大学学报(自然科学版)》2019,41(3):84-88

研究发现NH_2-MIL-101(Fe)金属有机框架材料可催化H_2O_2氧化3,3,5,5-四甲基联苯胺(TMB)显蓝色,表现出过氧化物模拟酶特性,而且在较宽的温度(4～80℃)及pH值范围(2～10)内保持其模拟酶活性,结合葡萄糖氧化酶,建立了测定葡萄糖的方法.在优化条件下,吸光度与葡萄糖浓度在0.75～50μmol/L范围内呈现良好的线性关系,对葡萄糖的检出限为0.75μmol/L.将本法用于血清中葡萄糖的测定,获得满意结果.  相似文献   

猕猴桃园套种蕺菜对土壤养分、酶活性及果实品质的影响     

李磊  龙友华  尹显慧  吴小毛  杨再福  张竹竹  舒然 《经济林研究》2019,37(3):128-137

为了提高猕猴桃果实产量与品质,在猕猴桃园以套种蕺菜、清耕和对照作为试验处理,测定不同时期猕猴桃根际土壤养分含量、微生物数量、酶活性和果实产量及品质,分析其相关性。结果表明:套种蕺菜后猕猴桃根际土壤碱解氮、速效磷、速效钾含量分别比对照处理提高13.95%、7.92%和3.94%,土壤细菌、真菌、放线菌数量分别提高19.01%、28.89%和16.32%,土壤过氧化氢酶、脲酶、蔗糖酶、磷酸酶活性分别提高17.02%、12.63%、17.57%和7.98%,单果质量和单位面积产量分别提高7.14%和7.68%,维生素C、干物质、可溶性固形物、可溶性总糖和可滴定酸含量分别提高7.97%、18.29%、2.09%、12.37%和14.18%。相关性分析结果表明,套种蕺菜后猕猴桃根际土壤速效钾含量与土壤中细菌数量、真菌数量、放线菌数量、脲酶活性、蔗糖酶活性、磷酸酶活性极显著正相关。土壤细菌数量与蔗糖酶活性显著正相关,与磷酸酶活性极显著正相关。土壤真菌数量与蔗糖酶活性极显著正相关。土壤放线菌数量与蔗糖酶活性、磷酸酶活性显著正相关。土壤速效磷含量与维生素C含量、可滴定酸含量极显著负相关,与干物质含量、可溶性固形物含量和可溶性总糖含量极显著正相关。土壤细菌数量、放线菌数量与维生素C含量极显著负相关。土壤真菌数量与维生素C含量显著负相关。土壤脲酶活性与干物质含量显著正相关,与可滴定酸含量显著负相关。维生素C含量与土壤蔗糖酶活性极显著负相关,与土壤磷酸酶活性显著负相关。套种蕺菜有利于提高猕猴桃根际土壤养分含量、微生物数量和酶活性,增加猕猴桃果实产量,改善猕猴桃果实品质。  相似文献   

Extraction and characterization of soil hydrogenases oxidizing atmospheric hydrogen     

Rongbo Guo  Ralf Conrad   《Soil biology & biochemistry》2008,40(5):1149-1154

Soils are the largest sink of atmospheric hydrogen contributing about 75% to the total budget. Atmospheric H₂ is assumed to be oxidized in soil by abiontic soil hydrogenases. Extraction of a forest soil with a slightly alkaline (pH 8.5) buffer containing polyethylene glycol (PEG), followed by filtration yielded a bacteria-free extract that oxidized H₂ at ambient concentrations (0.2–2.0 ppmv). Hydrogenase activity was assayed by gas chromatographic analysis of H₂ consumption and by conversion of ³H₂ to tritiated water. Only less than 2% of the original activity was recovered in the extract. Kinetic analysis nevertheless resulted in a biphasic kinetics exhibiting two K_m and V_max values that were similar to those detected in the original soil. In addition, activities of both original soil and soil extract showed similar optima at pH 4–6 and at 30 °C, indicating that representative fractions of soil hydrogenases were recovered in the extract. Precipitation with PEG or ultrafiltration allowed further purification of the activity, albeit only about 20% of that in the crude extract could be recovered in the precipitate or the fraction >100 kDa.  相似文献   

Response of an agricultural soil to pentachlorophenol (PCP) contamination and the addition of compost or dissolved organic matter   总被引：1，自引：0，他引：1  

Rosalia Scelza  Maria Antonietta Rao  Liliana Gianfreda   《Soil biology & biochemistry》2008,40(9):2162-2169

The response of a fresh, agricultural soil when contaminated with pentachlorophenol (PCP) and supplemented with compost (C) or dissolved organic matter (DOM) was studied in the laboratory. The concentration of PCP and the changes in various functionally related properties (i.e. microbial biomass, basal respiration, soil hydrolase and oxidoreductase activity) were measured over 150 d. Variations in the main physical and chemical properties of the soils were also monitored. Two different doses of compost (C1 = 0.27% and C2 = 0.83%, corresponding to 10 and 30 t ha⁻¹, respectively) or DOM (D1 = 0.07% and D2 = 0.2%) equivalent to the carbon content of the two compost doses C1 and C2 were used and the following five systems were investigated: soil (S), soil–compost (S-C1 and S-C2) and soil–DOM (S-D1 and S-D2). PCP concentrations declined progressively and significantly with time. This effect was most pronounced for the soils amended with the lower compost dose C1 (S-C1) and with the two DOM (S-D1 and S-D2) amounts. Significantly reduced amounts of PCP were extracted after its 500-d residence in the various systems. Higher amounts of the residual PCP were extracted from the humic acids (HA), fulvic acids (FA) and humin–mineral (HU) fractions of the 500 d aged samples than from the same unfractionated samples, indicating that the residual PCP preferentially accumulated in the organic fractions of soil. The soil showed an endogenous microbial activity as indicated by basal respiration, microbial biomass and all the enzymatic activities tested (dehydrogenase, glucosidase, phosphatase, arylsulphatase and urease). Addition of the PCP severely depressed some of the tested biochemical properties suggesting an inhibitory effect on microbial activity. Conversely, higher basal respiration, and similar β-glucosidase and phosphatase activities were measured in comparison with the controls. No significant effects were observed following the addition of two doses of the compost or the DOM. Fungal colonies belonging to the taxonomic group of Ascomycetes and identified as Byssochlamys fulva developed with time in all the PCP-contaminated samples. Growth of B. fulva in vitro in the presence of PCP showed that the isolate was tolerant to 12.5 and 25 mg l⁻¹ PCP and degraded 20% of its initial concentration in 8 d. Overall, the results indicate that many complex processes occurred in the contaminated soil and combinations of these determined the response to PCP contamination. The sorption of PCP to the soil matrix (which increased with time) and its degradation/transformation by indigenous soil microbial activity were likely involved. Both the processes appeared to be favoured by the presence of dissolved organic matter.  相似文献   

Emerging tools for measuring and modeling the in situ activity of soil extracellular enzymes     

Matthew D. Wallenstein  Michael N. Weintraub   《Soil biology & biochemistry》2008,40(9):2098-2106

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Dynamics of upward and downward N₂O and CO₂ fluxes in ploughed or no-tilled soils in relation to water-filled pore space, compaction and crop presence     

B.C. Ball  I. Crichton  G.W. Horgan 《Soil & Tillage Research》2008,101(1-2):20-30

Sharp peaks in nitrous oxide (N₂O) fluxes under no-tillage in wet conditions appear to be related to near surface soil and crop cover conditions. Here we explored some of the factors influencing tillage effects on short-term variations in gas flux so that we could learn about the mechanisms involved. Field investigations revealed that a cumulative emission of 13 kg N₂O–N ha⁻¹ over a 12-week period was possible under no-tillage for spring barley. We investigated how reducing crop cover and changing the structural arrangement of the water-filled pore space (WFPS) by short-term laboratory compaction influenced N₂O and carbon dioxide (CO₂) fluxes in upward and downward directions in core samples from tilled and untilled soil. Increasing the downward flux of N₂O within a soil profile by changing soil or moisture conditions may increase the likelihood of its further reduction to N₂ or dissolution. We took undisturbed cores from 3 to 8 cm depth, equilibrated them to −1 or −6 kPa matric potential, incubated them and measured N₂O and CO₂ fluxes from the upper and lower surfaces in a purpose-designed apparatus before and after compaction in an uniaxial tester. We also measured WFPS, air permeability, bulk density and air-filled porosity before and after compaction. Spring barley was tested in 1999 and winter barley in 2000.Fluxes of N₂O were from 1.5 to 35 times higher from no-tilled than ploughed even where the soil was of similar bulk density. Reduction of the crop cover increased CO₂ flux and could reduce N₂O flux. The effects of structural changes induced by laboratory compaction on the fluxes of N₂O and CO₂ were not influenced greatly by the tillage and crop cover treatments. Fluxes from the upper surfaces of cores (corresponding to 3 cm soil depth, upwards direction) could be up to 100 times greater (N₂O) or 8 times (CO₂) than from the lower surfaces (8 cm depth, downwards direction). These differences between surfaces were greatest when N₂O fluxes were very high in no-tilled soil (4.2 mg N₂O–N m⁻² h⁻¹) as occurred when WFPS exceeded 80% or became blocked with water, an effect that was increased by our compaction treatment. In general N₂O fluxes increased with WFPS. The production and emission of N₂O were strongly influenced by the soil physical environment, the magnitude of the water-filled pore space and continuity of the air-filled pore space in particular, produced in no-till versus plough cultivation.  相似文献   

Soil chemical and microbiological properties along a chronosequence of Caragana microphylla Lam. plantations in the Horqin sandy land of Northeast China   总被引：1，自引：0，他引：1  

Chengyou Cao  Deming Jiang  Xiaohui Teng  Yong Jiang  Wenju Liang  Zhenbo Cui 《Applied soil ecology》2008,40(1):78-85

Caragana microphylla Lam., a leguminous shrub, is a dominant native plant species widely planted to stabilize the moving and semi-moving sand dunes in the semi-arid Horqin sandy land of Northeast China. The objective of this study was to determine how C. microphylla plantations affected the physical, chemical and microbiological properties of a sandy soil. Soil samples at the depths of 0–10, 10–20, 20–30, 30–40, and 40–50 cm were collected from the C. microphylla plantations with an age sequence of 0, 5, 10, and 23 years. The results showed that shrub growth altered microclimate, increased litter input, and hence, improved soil water holding capacity, contents of total carbon, total N and microbial biomass C and N, electrical conductivity, and activities of urease, phosphomonoesterase, protease, dehydrogenase and polyphenol oxidase, and decreased soil bulk density. These trends increased with increasing plantation age but decreased with increasing soil depth. C. microphylla establishment could be an effective and applicable measure to restore vegetation and control desertification in the Horqin sandy land, and recommended for adoption in semi-arid sandy areas on a large scale.  相似文献   

黄河首曲重大生态功能区护岸林建设问题探讨   总被引：3，自引：0，他引：3  

陈文业  戚登臣  郑华平  李广宇  刘正恒  宗文杰  杨鑫光  陈炜青  王芳 《水土保持研究》2008,(6)

分析了河岸防护林改变区域小气候、巩固河岸、保持水土、防风固沙、改良土壤、湿地保护、提供饲料、薪材和增加收入、提高畜牧业生产力、丰富和改善高寒区景观等作用,系统阐述了加强河岸防护林建设的重要性,针对性地提出了河岸防护林树种组成单一、体系结构不够完整、自然因素恶劣等护岸林建设问题,并提出了进一步发展建设的对策,在黄河首曲重大生态功能区的环境建设中加强黄河护岸林建设,对于黄河首曲生态环境的治理、恢复、重建和改善具有十分重要的意义。  相似文献   

长期有机无机肥配施对褐土微生物生物量碳、氮量及酶活性的影响   总被引：3，自引：0，他引：3  

贾伟  周怀平  解文艳  关春林  郜春花  石彦琴 《植物营养与肥料学报》2008,14(4):700-705

通过对山西省寿阳长期定位试验田0―20 cm和20―40 cm的土壤测定和分析,探讨了长期有机无机肥配施下褐土微生物生物量碳、氮和酶活性的变化以及相关性。结果表明,褐土微生物生物量C、N变化基本一致。褐土微生物生物量碳、氮从0―20 cm到20―40 cm土层均呈减少趋势;长期单施高量有机肥、有机无机肥合理配施都能提高褐土微生物生物量碳、氮;不同用量的长期单施化肥处理不能使微生物生物量C、N显著增加。脲酶和碱性磷酸酶活性从0―20 cm到20―40 cm土层呈减少趋势;长期单施高量有机肥和有机无机肥合理配施可使褐土脲酶及碱性磷酸酶活性增加。脲酶活性随单施化肥量的增加有变大趋势,而碱性磷酸酶活性则呈变小趋势。土壤微生物量碳氮、土壤酶活性及土壤养分之间的显著相关性表明,微生物生物量C、N和土壤酶活性可以判断褐土土壤有机质和N素状况,可作为评价褐土土壤肥力水平和土壤培肥效果的生物学指标,同时也可为提高褐土土壤肥力水平和土壤培肥效果提供依据。  相似文献   

流动沙丘先锋植物沙米的生态防护作用   总被引：3，自引：0，他引：3  

马全林  王继和  张景光  詹科杰  张德魁  陈芳 《水土保持学报》2008,22(1):140-145

使用野外风速廓线仪与阶梯式集沙仪,对流动沙丘先锋植物沙米及其群落的生态防护作用进行了野外实地观测研究。研究结果表明,沙米植株成塔状,基部分枝,株高变异性、可塑性大,与其他形态指标呈显著正相关,通过测定株高可掌握其基本形态特征。立枯沙米单株可降低风速90%以上,并能阻挡风沙流形成沙舌,沙舌积沙量、高度、长度与沙米体积、高度和冠幅呈显著相关。沙米群落粗糙度达到6.325 cm,是裸露流沙区的2635倍。在裸露流沙区200 cm高度风速为6.2 m/s时,裸露流沙区输沙量达到86.34 g/cm.h,而沙米群落中无风沙流发生;风速为9.5 m/s时,裸露流沙区输沙量也达到沙米群落的574倍。研究认为,在短期(2~3年)和局部空间范围(流动沙丘坡脚与两翼以及裸沙斑块),立枯沙米及其群落具有较明显的防风固沙作用;发达的生殖生长、侧枝系统和侧根系统,枯死后可保留2~3个生长季,是沙米发挥防风固沙作用的关键所在。  相似文献