Fluorescence of raw cane sugars evaluated by chemometrics     

Baunsgaard D  Nørgaard L  Godshall MA 《Journal of agricultural and food chemistry》2000,48(10):4955-4962

In a fluorescence study of raw cane sugar samples, two-way and three-way chemometric methods have been used to extract information about the individual fluorophores in the sugar from fluorescence excitation-emission landscapes. A sample set of 47 raw sugar samples representing a varied selection was analyzed, and three individual fluorophores with (275, 350) nm, (340, 420) nm, and (390, 460) nm as their approximate excitation and emission maxima were found. The spectral profiles of the fluorophores were estimated with the three-way decomposition model PARAFAC. Two-way principal component analysis (PCA) of unfolded fluorescence landscapes confirmed the PARAFAC results and showed patterns of samples related to time of storage. Partial least squares (PLS) calibration models of color at 420 nm had a high model error due to the very high color range of the raw sugars, but variable selection performed on the fluorescence data revealed that all three fluorophores were correlated to color. The (275, 350) nm fluorophore is considered as a color precursor to the color developed on storage and the (340, 420) nm and (390, 460) nm fluorophores show colorant polymer characteristics.  相似文献   

The N₂O product ratio of nitrification and its dependence on long-term changes in soil pH   总被引：1，自引：0，他引：1  

Pål Tore Mørkved  Peter Dörsch 《Soil biology & biochemistry》2007,39(8):2048-2057

The contribution of nitrification to the emission of nitrous oxide (N₂O) from soils may be large, but its regulation is not well understood. The soil pH appears to play a central role for controlling N₂O emissions from soil, partly by affecting the N₂O product ratios of both denitrification (N₂O/(N₂+N₂O)) and nitrification (N₂O/(NO₂⁻+NO₃⁻). Mechanisms responsible for apparently high N₂O product ratios of nitrification in acid soils are uncertain. We have investigated the pH regulation of the N₂O product ratio of nitrification in a series of experiments with slurries of soils from long-term liming experiments, spanning a pH range from 4.1 to 7.8. ¹⁵N labelled nitrate (NO₃⁻) was added to assess nitrification rates by pool dilution and to distinguish between N₂O from NO₃⁻ reduction and NH₃ oxidation. Sterilized soil slurries were used to determine the rates of chemodenitrification (i.e. the production of nitric oxide (NO) and N₂O from the chemical decomposition of nitrite (NO₂⁻)) as a function of NO₂⁻ concentrations. Additions of NO₂⁻ to aerobic soil slurries (with ¹⁵N labelled NO₃⁻ added) were used to assess its potential for inducing denitrification at aerobic conditions. For soils with pH?5, we found that the N₂O product ratios for nitrification were low (0.2-0.9‰) and comparable to values found in pure cultures of ammonia-oxidizing bacteria. In mineral soils we found only a minor increase in the N₂O product ratio with increasing soil pH, but the effect was so weak that it justifies a constant N₂O product ratio of nitrification for N₂O emission models. For the soils with pH 4.1 and 4.2, the apparent N₂O product ratio of nitrification was 2 orders of magnitude higher than above pH 5 (76‰ and 14‰). This could partly be accounted for by the rates of chemodenitrification of NO₂⁻. We further found convincing evidence for NO₂⁻-induction of aerobic denitrification in acid soils. The study underlines the role of NO₂⁻, both for regulating denitrification and for the apparent nitrifier-derived N₂O emission.  相似文献   

Enzymatic solubilization of arabinoxylans from native, extruded, and high-shear-treated rye bran by different endo-xylanases and other hydrolyzing enzymes     

Figueroa-Espinoza MC  Poulsen C  Borch Søe J  Zargahi MR  Rouau X 《Journal of agricultural and food chemistry》2004,52(13):4240-4249

The overall objective of this research was to find a new way to valorize rye bran, by producing a gellifier from the enzymatic solubilization of arabinoxylans (AX). The effects of three pure endo-xylanases from Aspergillus niger (Xyl-1), Talaromyces emersonii (Xyl-2), and Bacillus subtilis (Xyl-3) and of Grindamyl S100 (GS100), a commercial enzyme preparation containing a Xyl-1 type endo-xylanase, were tested on rye bran to study the solubilization of water-unextractable arabinoxylans (WUAX). Eight different extrusion-treated rye brans were also used as substrates to find the best physical treatment to facilitate enzymatic arabinoxylan (AX) solubilization. Arabinoxylans were better solubilized from the bran extruded at high temperature using Xyl-3. This enzyme was then tested in combination with pure (1,4)-beta-d-arabinoxylan arabinofuranohydrolase (AXH) and endo-beta-d-glucanase or ferulic acid esterase (FAE), from A. niger. Only beta-glucanase in combination with Xyl-3 improved the AX extraction, but it did not have a marked effect on the viscosity of the extracts. Xyl-3 was then tested on a high-shear-treated rye bran, and results were compared to those obtained with the high-temperature-extruded rye bran. The high-shear treatment did not improve the bran AX enzymatic solubilization. The combination of FAE with Xyl-1 or Xyl-3 did not improve the AX extraction from untreated and high-shear-treated rye bran. Finally, to study the gelation capacity of the enzymatically solubilized AX, the effect of the hydrogen peroxide/horseradish peroxidase (H(2)O(2)/POD) was tested on the Xyl-3 high-temperature-extruded bran extracts. Solubilized AX did not gel in the presence of the oxidizing system.  相似文献   

Flavone C-glycoside,phenolic acid,and nitrogen contents in leaves of barley subject to organic fertilization treatments   总被引：1，自引：0，他引：1  

Nørbaek R  Aaboer DB  Bleeg IS  Christensen BT  Kondo T  Brandt K 《Journal of agricultural and food chemistry》2003,51(3):809-813

From the leaves of barley, Hordeum vulgare, one new flavone C-glucoside and three known flavone glucosides were isolated and characterized by (1)H and (13)C NMR and MALDI-TOF-MS. The novel flavone C-glucoside was isovitexin 7-O-beta-[6' "-O-(E)-p-coumaroyl]glucoside (6' "-coumaroylsaponarin), and the known compounds were isovitexin 7-O-beta-[6' "-O-(E)-feruloyl]glucoside, isoorientin 7-O-beta-[6' "-O-(E)-feruloyl]glucoside, and tricin 7-O-beta-glucoside. The sum of all the flavone glycosides and soluble phenolic acids in the leaves decreased with increased rate of plant nutrients given in animal manure and with increased crop yield. All of the major phenylpropanoids showed the same general response to nutrient level. The concentration of nitrogen in the leaves was not directly related to nutrient application or to contents of phenylpropanoids.  相似文献   

Assessment of C budget for grasslands and drylands of the world   总被引：1，自引：0，他引：1  

Dennis S. Ojima  Bjørn O. M. Dirks  Edward P. Glenn  Clenton E. Owensby  Jonathan O. Scurlock 《Water, air, and soil pollution》1993,70(1-4):95-109

Intergovernmental Panel on Climate Change (IPCC) estimates indicate that potential changes in seasonal rainfall and temperature patterns in central North America and the African Sahel will have a greater impact on biological response (such as plant production and biogeochemical cycling) and feedback to climate than changes in the overall amount of annual rainfall. Simulation of grassland and dryland ecosystem responses to climate and CO₂ changes demonstrates the sensitivity of plant productivity and soil C storage to projected changes in precipitation, temperature and atmospheric CO₂. Using three different land cover projections, changes in C levels in the grassland and dryland regions from 1800 to 1990 were estimated to be ?13.2, ?25.5 and ?14.7 Pg, i.e., a net source of C due to land cover removal resulting from cropland conversion. Projections into the future based on a double-CO₂ climate including climate-driven shifts in biome areas by the year 2040 resulted in a net sink of +5.6, +27.4 and +26.8 Pg, respectively, based upon sustainable grassland management. The increase in C storage resulted mainly from an increase in area for the warm grassland sub-biome, together with increased soil organic matter. Preliminary modeling estimates of soil C losses due to 50 yr of regressive land management in these grassland and dryland ecoregions result in a 11 Pg loss relative to current conditions, and a potential loss of 37 Pg during a 50 yr period relative to sustainable land-use practices, an average source of 0.7 Pg C yr^?1. Estimates of the cost of a 20 yr rehabilitation program are 5 to 8×10⁹ US$ yr^?1, for a C sequestering cost of approximately 10 US$ per tC.  相似文献   

Lysosomal Fragility in Earthworms (Eisenia Veneta) Exposed to Heavy Metal Contaminated Soils from Two Abandoned Pyrite Ore Mines in Southern Norway     

Hønsi  Torunn G.  Stubberud  Hege E.  Andersen  Sjur  Stenersen  Jørgen 《Water, air, and soil pollution》2003,142(1-4):27-37

In this study we have investigated the toxicity of soils from thetwo abandoned pyrite mines Ertelien and Konnerud in the southernpart of Norway. Soil samples were collected close to the pitheadof the mines, and earthworms were exposed to different concentrations of the contaminated mine soil mixed with commercial plant soil for a period of 14 days. Life-cycle responses such as growth and survival, as well as the biomarkerresponse lysosomal fragility were measured. The body burdens ofthe four heavy metals Cu, Cd, Zn and Pb were detected in the worms, and the body concentration of the metals generally increased with increasing heavy metal concentration in the soil.The growth and mortality of the earthworms were not influenced when exposed to any of the mine soil concentrations used. The lysosomal fragility of the earthworm coelomocytes measured by the neutral red retention time (NRR-time) was found to be markedly reduced in all the exposed earthworms. This assay seemsto be a sensitive and dose dependent endpoint for the toxicity assessment of heavy metal mixtures in pyrite mine soils.  相似文献   

Arginine ammonification assay as a rapid index of gross N mineralization in agricultural soils     

Torben A. Bonde  Tommy Nielsen  Morten Miller  Jan Sørensen 《Biology and Fertility of Soils》2001,34(3):179-184

Seasonal dynamics of in situ gross nitrogen (N) mineralization rates were measured using the ¹⁵N-NH₄⁺ isotope dilution method in a Danish soil subjected to four different agricultural practices (set aside, barley, winter wheat and clover). Results were compared to arginine ammonification in the soil samples measured as NH₄⁺ production following addition of excess (1 mM) arginine. In the set aside, barley, winter wheat and clover soils the average annual rates of gross N mineralization (0.29, 0.60, 1.34 and 1.75 µg NH₄⁺-N g^-1 day^-1, respectively) and arginine ammonification activity (0.21, 0.55, 0.88, and 1.33 µg NH₄⁺-N g^-1 h^-1, respectively) were well correlated. Furthermore, the seasonal variations of gross N mineralization and arginine ammonification activities were very similar, showing rapid responses to rainfall and generally higher activities in wetted soils. As tested in the laboratory, the arginine ammonification activity correlated well with heterotrophic microbial respiration activity (CO₂ production) in soil samples and further displayed a simple, one-component Michaelis-Menten kinetics with a high affinity for arginine (K_m value of 48 µM LJ µM) as determined from non-linear parameter estimation. This indicated that arginine ammonification activity was primarily due to microorganisms, and the activity was also shown to be at a minimum in sterile soil samples. All evidence thus supported that our standard assay of arginine ammonification activity provides a good index of gross N mineralization rates by the microorganisms in soil under in situ conditions.  相似文献   

Decrease in Acid Deposition - Recovery in Norwegian Waters     

Brit Lisa Skjelkvåle  Kjetil Tørseth  Wenche Aas  Tom Andersen 《Water, air, and soil pollution》2001,130(1-4):1433-1438

Concentrations of sulphate in precipitation in southern Norway have decreased by 50–60% from 1980–1999. This has caused a decrease in sulphate concentrations in lakes of 30–40% from 1986–1999. Nitrogen in precipitation has decreased slightly over the last 10-years. In lakewater there has also been a significant but slight decrease. Concentrations of non-marine base cations in precipitation have decreased by 40% from 1980–1999. In lakewater, non-marine base cation concentrations have been at about the same level the last 10 years. This indicates that acid deposition has decreased sufficiently such that the pool of exchangeable base cations in the soil is now being replenished. The acidification situation in lakes in Norway has thus shown a clear improvement over the last 8–10 years. pH, alkalinity and ANC (acid neutralising capacity) have all increased. Concentrations of inorganic (toxic) aluminium species have decreased. The trends in H⁺ and Alⁿ⁺ do not follow the relation expected if Alⁿ⁺ concentrations were governed solely by a single solid phase of Al(OH)₃.  相似文献   

Mineralization of carbon and nitrogen from fresh and anaerobically stored sheep manure in soils of different texture   总被引：1，自引：0，他引：1  

Peter Sørensen  Erik Steen Jensen 《Biology and Fertility of Soils》1995,19(1):29-35

A sandy loam soil was mixed with three different amounts of quartz sand and incubated with (¹⁵NH₄)₂SO₄ (60 g N g^-1 soil) and fresh or anaerobically stored sheep manure (60 g g^-1 soil). The mineralization-immobilization of N and the mineralization of C were studied during 84 days of incubation at 20°C. After 7 days, the amount of unlabelled inorganic N in the manure-treated soils was 6–10 g N g^-1 soil higher than in soils amended with only (¹⁵NH₄)₂SO₄. However, due to immobilization of labelled inorganic N, the resulting net mineralization of N from manure was insignificant or slightly negative in the three soil-sand mixtures (100% soil+0% quartz sand; 50% soil+50% quartz sand; 25% soil+75% quartz sand). After 84 days, the cumulative CO₂ evolution and the net mineralization of N from the fresh manure were highest in the soil-sand mixutre with the lowest clay content (4% clay); 28% fo the manure C and 18% of the manure N were net mineralized. There was no significant difference between the soil-sand mixtures containing 8% and 16% clay, in which 24% of the manure C and -1% to 4% of the manure N were net mineralized. The higher net mineralization of N in the soil-sand mixture with the lowest clay content was probably caused by a higher remineralization of immobilized N in this soil-sand mixture. Anaerobic storage of the manure reduced the CO₂ evolution rates from the manure C in the three soil-sand mixtures during the initial weeks of decomposition. However, there was no effect of storage on net mineralization of N at the end of the incubation period. Hence, there was no apparent relationship between net mineralization of manure N and C.  相似文献   

Differentiation of species from the Penicillium roqueforti group by volatile metabolite profiling   总被引：1，自引：0，他引：1  

Karlshøj K  Larsen TO 《Journal of agricultural and food chemistry》2005,53(3):708-715

Species from the Penicillium roqueforti group were differentiated by volatile metabolite profiling primarily of sesquiterpenes. A total of 24 isolates from species P. roqueforti, Penicillium carneum, and the recently described species Penicillium paneum were inoculated on yeast extract sucrose agar. Volatile metabolites were collected by diffusive sampling onto tubes containing Tenax TA, overnight between the fifth and sixth days of incubation. Volatiles were thermally desorbed and analyzed by gas chromatography coupled to mass spectrometry. The sesquiterpene area of the chromatogram was investigated, and potential sesquiterpenes were tabulated by comparison of their Kovats retention index and mass spectrum. In general, P. carneum isolates produced the lowest number of sesquiterpenes, all of which were unique for P. carneum within the P. roqueforti group. P. roqueforti and P. paneum produced a larger variety of volatile metabolites, some of which they have in common and some of which are unique for the two species. (+)-Aristolochene was found in samples from P. paneum and P. roqueforti. Other Penicillium species in which (+)-aristolochene was also detected were P. commune, P. glandicola, and P. solitum.  相似文献