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  • 1
    Electronic Resource
    Electronic Resource
    AMINO ALCOHOLS. I. PHENYLPROPANOLAMINE AND PARA-TOLYLPROPANOLAMINE (1929)
    s.l. : American Chemical Society
    Journal of the American Chemical Society 51 (1929), S. 2262-2266 
    Details
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ja01382a044
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  • 2
    Electronic Resource
    Electronic Resource
    A NEW SERIES OF ANESTHETICS. ACYLANILINE DERIVATIVES (1929)
    s.l. : American Chemical Society
    Journal of the American Chemical Society 51 (1929), S. 2570-2574 
    Details
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ja01383a043
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  • 3
    Electronic Resource
    Electronic Resource
    THE QUANTITATIVE DETERMINATION OF MORPHINE IN THE VARIOUS ORGANS WHEN INJECTED INTO CATS AND RABBITS. (1916)
    s.l. : American Chemical Society
    Journal of the American Chemical Society 38 (1916), S. 1873-1876 
    Details
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ja02266a024
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  • 4
    Electronic Resource
    Electronic Resource
    Morphological and anatomical characterisation of black alder Alnus glutinosa (L.) Gaertn. ectomycorrhizas (1997)
    Springer
    Mycorrhiza 7 (1997), S. 201-216 
    Details
    ISSN: 1432-1890
    Keywords: Key words Alder mycorrhizas ; Characterisation of ectomycorrhizas ; Morphology ; Anatomy ; Alnus glutinosa
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract  Ectomycorrhizal types of black alder [Alnus glutinosa (L.) Gaertn.] collected over a 3-year period within an alder forest were characterised by morphological and anatomical features. Of the total of 16 types, 14 are described for the first time in this paper. Eight identified types belong to the genera Russula, Lactarius, Naucoria, and Cortinarius, while eight further types remained unidentified. In some cases, similarities of mantle features indicate relationships to identified mycorrhizas. Mycorrhizas of Naucoria escharoides and N. subconspersa were not distinguished. Two unidentified mycorrhizal types exhibited hyphal mantle structures very similar to these Naucoria species. Within the genus Cortinarius, mycorrhizas of C. cf. helvelloides were easily distinguished from all other Cortinarius-like mycorrhizas described on Alnus, which in general showed little anatomical variation. Two further unidentified mycorrhizas, "Alnirhiza lilacina" and "A. violacea", probably also belong to Cortinarius. The ectomycorrhiza of Russula pumila was the only identified type within the genus Russula, but the unidentified type "Alnirhiza cremicolor" also likely belongs to this genus. Three Lactarius species were present in the experimental plot. Two species (L. obscuratus and L. omphaliformis) had indistinguishable mycorrhizal types, but were easily differentiated from the mycorrhizas of L. lilacinus, which caused intracellular penetration of Hartig net hyphae into epidermal and cortical cells. All other mycorrhizal types of black alder exhibited a paraepidermal Hartig net without penetration of root cells. Two unidentified mycorrhizal types "Alnirhiza atroverrucosa" and "A. cystidiobrunnea", already described from North American Alnus rubra as unnamed morphotypes, showed no similarity to identified mycorrhizas. All 16 mycorrhizal types appeared to be specific or at least typical for alders, since they have not yet been reported from other tree species.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s005720050182
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  • 5
    Electronic Resource
    Electronic Resource
    Enhancing the mineralization of [U-14C]dibenzo-p-dioxin in three different soils by addition of organic substrate or inoculation with white-rot fungi (1997)
    Springer
    Applied microbiology and biotechnology 48 (1997), S. 665-670 
    Details
    ISSN: 1432-0614
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: Abstract The potential for aerobic mineralization of [U-14C]dibenzo-p-dioxin (DD) was investigated in samples of three different agricultural soils already contaminated with polychlorinated dibenzo-p-dioxins and dibenzofurans (PCDD/F) by industrial activities. The influence of amendments, i.e. wheat straw and compost, and of soil treatment by inoculation with lignolytic fungi, grown on wheat straw substrate, was tested. All the soils tested contained an indigenous DD-mineralizing microflora. The soil characterized by the highest organic matter content and the highest content of soil microbial biomass displayed the best DD mineralization of 36.6% within 70 days, compared with the two organic-matter-poor soils with an endogenous DD mineralization of 19.5% and 23.3% respectively. Amendments with compost increased DD mineralization up to 28% in both soils with low organic matter and microbial biomass content, but did not affect mineralization in the organic-matter-rich soil. Addition of wheat straw had no constant influence on DD mineralization in the soils tested. The best DD mineralization resulted from inoculation with lignolytic white-rot fungi (Phanerochaete chrysosporium, Pleurotus sp. Florida, Dichomitus squalens) and with an unidentified lignolytic fungus, which was isolated originally from a long-term PCDD/F-contaminated soil. A mineralization of up to 50% within 70 days was reached by this treatment. The influence of inoculated fungi on mineralization differed between the soils investigated.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s002530051113
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  • 6
    Electronic Resource
    Electronic Resource
    Initiation of [36Cl]hexachlorobenzene dechlorination in three different soils under artificially induced anaerobic conditions (1997)
    Springer
    Applied microbiology and biotechnology 48 (1997), S. 115-120 
    Details
    ISSN: 1432-0614
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: Abstract The potential for reductive dechlorination of hexachlorobenzene was investigated in samples of three different, naturally oxic soils held under conditions of high oxygen deficiency. The soils were water-saturated and the influence on dechlorination of adding different electron donors, a surfactant and an anaerobic microbial consortium was tested. The influence of supplied electron donors seems to depend on the organic matter content of the soils. Dechlorination in the organic-matter-rich soil from Maulach was not affected by amendment with organic electron donors. A release of about 40% chloride within 140 days was observed for this soil in all biotic-treated assays. By contrast, the organic-matter-poor soil of Eppingen showed no dechlorination in unamended assays. However, when it was supplemented with organic electron donors dechlorination of 2%–37% occurred within 140 days, depending on the type of electron donor. Complex substrate (wheat strawdust), from which carbon is slowly liberated, gave the best results. These two soils had an indigenous dechlorinating anaerobic microflora, whereas the third soil (Rastatt) required inoculation with an anaerobic consortium for dechlorination. The addition of electron donors alone did not cause dechlorination in this sandy soil. The addition of a surfactant (Tween 80) to increase the bioavailability of hexachlorobenzene did not enhance dechlorination. This process was not inhibited by inherent alternative electron acceptors in soil (NO3−, SO4 2−, Fe3+). The dechlorination did not require methanogenic conditions.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s002530051025
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  • 7
    Electronic Resource
    Electronic Resource
    Ratios between estimates of microbial biomass content and microbial activity in soils (1998)
    Springer
    Biology and fertility of soils 27 (1998), S. 374-379 
    Details
    ISSN: 1432-0789
    Keywords: Key words Arginine-ammonification rate ; Microbial biomass content ; Microbial activities ; Metabolic quotient ; Ecosystem research
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  The content levels and activities of the microbiota were estimated in topsoils and in one soil profile at agricultural and forest sites of the Bornhöved Lake district in northern Germany. Discrepancies between data achieved by fumigation-extraction (FE) and substrate-induced respiration (SIR), both used for the quantification of microbial biomass, were attributed to the composition of the microbial populations in the soils. In the topsoils, the active, glucose-responsive (SIR) versus the total, chloroform-sensitive microbial (FE) biomass decreased in the order; field maize monoculture (field-MM)〉field crop rotation (field-CR) and dry grassland〉beech forest. This ratio decreased within the soil profile of the beech forest from the litter horizon down to the topsoil. Differences between microbial biomass and activities suggested varying biomass-specific transformation intensities in the soils. The metabolic quotient (qCO2), defined as the respiration rate per unit of biomass, indicates the efficiency in acquiring organic C and the intensity of C mineralization, while biomass-specific arginine-ammonification (arginine-ammonification rate related to microbial biomass content) seems to be dependent on N availability. The qCO2, calculated on the basis of the total microbial biomass, decreased for the topsoils in the same order as did the ratio between the active, glucose-responsive microbial biomass to the total, chloroform-sensitive microbial biomass, in contrast to qCO2 values based on the glucose-responsive microbial biomass, which did not. There was no difference between the levels of biomass-specific arginine-ammonification in topsoils of the fertilized field-CR, fertilized field-MM, fertilized dry grassland and eutric alder forest, but levels were lower in the beech forest, dystric alder forest, and unfertilized wet grassland topsoils. Ratios between values of different microbiological features are suggested to be more useful than microbiological features related to soil weight when evaluating microbial populations and microbially mediated processes in soils.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s003740050446
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  • 8
    Electronic Resource
    Electronic Resource
    Ecological pre-release risk assessment of two genetically engineered, bioluminescent Rhizobium meliloti strains in soil column model systems (1997)
    Springer
    Biology and fertility of soils 25 (1997), S. 340-348 
    Details
    ISSN: 1432-0789
    Keywords: Key wordsRhizobium meliloti ; Genetically engineered microorganisms ; Ecological risk assessment ; Soil column model system ; Polymerase chain reaction
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract In order to identify potential ecological risks associated with the environmental release of two Rhizobium meliloti strains, genetically engineered with the firefly-derived luciferase gene (luc), a pre-release greenhouse investigation was conducted. The upper 4 cm of soil columns (30 cm diameter; 65 cm depth), which were filled according to the horizons of an agricultural field (loamy sand), were inoculated with seeds of Medicago sativa (alfalfa) and R. meliloti cells at approximately 5×106 cells·g–1 soil. Four treatments were tested: inoculation with a non-engineered wild type strain (2011), strain L33 (luc +), strain L1(luc +, recA–) and non-inoculated controls. The fate of the engineered strains was followed by two methods: (1) selective cultivation and subsequent detection of bioluminescent colonies and (2) PCR detection of the luc gene in DNA, directly extracted from soil. Strain R. meliloti L33 declined to 9.0×104 cfu·g–1 soil within 24 weeks and to 2.8×103 cfu·g–1 soil within 85 weeks in the upper 25 cm of the soil columns. Decline rates for R. meliloti L1 were not significantly different. Vertical distribution analysis of the recombinant cells after 37 weeks revealed that in three of four columns tested, the majority of cells (〉98%) remained above 10 cm soil depth and no recombinant cells occurred below 20 cm depth. However, in one column all horizons below 20 cm were colonized with 2.2×104 to 6.8×104 cfu g–1 soil. Ecological monitoring parameters included organic substance, total nitrogen, ammonium and nitrate, microbial biomass, culturable bacteria on four different growth media and the immediate utilization of 95 carbon sources (BiologGN) by soil-extracted microbial consortia. None of the parameters was specifically affected by the genetically engineered cells.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s003740050323
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  • 9
    Electronic Resource
    Electronic Resource
    Nitrous oxide emissions from a fallow and wheat field as affected by increased soil temperatures (1998)
    Springer
    Biology and fertility of soils 27 (1998), S. 307-314 
    Details
    ISSN: 1432-0789
    Keywords: Key words Global warming ; Nitrous oxide ; Soil warming ; Agriculture ; Ecosystem manipulation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  In order to determine the effects of increased soil temperature resulting from global warming on microbiological reactions, a 21-month field experiment was carried out in the Bavarian tertiary hills. The major objective was to focus on N2O releases as either a positive or negative feedback in response to global warming. The soils of a fallow field and a wheat field were heated 3  °C above ambient temperature and N2O fluxes were measured weekly from June 1994 to March 1996. During the experimental period, measured temperature differences between the control plots and the heated plots were 2.9±0.3  °C at a depth of 0.01 m and 1.0–1.8  °C at a depth of 1 m. Soil moisture decreased with the elevated soil temperatures of the heated plots. The mean differences in soil moisture between the treatments were 6.4% (fallow field) and 5.2%DW (wheat field dry weight, DW), respectively. Overall N2O releases during the experimental period from the fallow field were 4.8 kg N2O–N ha–1 in the control plot against 5.0 kg N2O–N ha–1 in the heated plot, and releases from the wheat field were 8.0 N2O–N ha–1 in the control plot and 7.6 N2O–N kg ha–1 in the heated plot. However, on a seasonal basis, cumulated N2O emissions differed between the plots. During the summer months (May–October), releases from the heated fallow plot were 3 times the rates from the control plot. In the winter months, N2O releases increased in both the fallow and wheat fields and were related to the number of freezing and thawing cycles.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s003740050438
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  • 10
    Electronic Resource
    Electronic Resource
    Nitrous oxide release from arable soil: importance of perennial forage crops (1998)
    Springer
    Biology and fertility of soils 28 (1998), S. 36-43 
    Details
    ISSN: 1432-0789
    Keywords: Key words Nitrous oxide ; Forage crops ; Spring barley ; Nitrogen fertiliser ; Thawing and freezing cycles
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  N2O emission rates from a sandy loam soil were measured in a field experiment with 2 years of perennial forage crops (ryegrass, ryegrass-red clover, red clover) and 1 year of spring barley cultivation. Spring barley was sown after the incorporation of the forage crop residues. All spring barley plots received 40 kg N ha–1 N fertiliser. Ryegrass, ryegrass-red clover and red clover plots were fertilised with 350 kg N ha–1, 175 kg N ha–1 and 0 kg N ha–1, respectively. From June 1994 to February 1997, N2O fluxes were continuously estimated using very large, closed soil cover boxes (5.76 m2). In order to compare the growing crops, the 33 months of investigation were separated into three vegetation periods (March–September) and three winter periods (October–February). All agronomic treatments (fertilisation, harvest and tillage) were carried out during the vegetation period. Large temporal changes were found in the N2O emission rates. The data were approximately log-normally distributed. Forty-seven percent of the annual N2O losses were observed to occur during winter, and mainly resulted from N2O production during daily thawing and freezing cycles. No relationship was found between the N2O emissions during the winter and the vegetation period. During the vegetation period, N2O losses and yields were significantly different between the three forage crops. The unfertilised clover plot produced the highest yields and the lowest N2O losses on this soil compared to the highly fertilised ryegrass plot. Total N2O losses from soil under spring barley were higher than those from soil under the forage crops; this was mainly a consequence of N2O emissions after the incorporation of the forage crop residues.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s003740050460
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