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991.
Silke Ruppel Vigdis Torsvik Frida Lise Daae Lise Øvreås Jörg Rühlmann 《Biology and Fertility of Soils》2007,43(4):449-459
In this study, the interrelation between nitrogen availability and prokaryotic diversity are studied using a well-characterised
system from a long-term field experiment on a loamy sandy soil. The prokaryotic potential functional diversity and community
composition were assessed using community-level physiological profiling (CLPP), and their phylogenetic diversity was analysed
using polymerase chain reaction-denaturing gradient gel electrophoresis (PCR-DGGE) in combination with sequencing analysis.
Highest prokaryotic potential functional diversity was measured in the control soil receiving no N fertilisation, indicating
an efficient as well as versatile utilisation of the substrates in this soil. Both substrate utilisation richness and substrate
utilisation evenness, the two constituents of the functional diversity, were decreased with increasing N supply. Furthermore,
distinct prokaryotic community compositions were generated in N-enriched soils compared to unfertilised control soils. These
differences suggest a dominance of populations adapted to utilising readily available substrates. We demonstrated that the
shift in prokaryotic functional diversity was connected to a shift in the phylogenetic structure of the bacterial and archaeal
communities. Taken together, our data clearly show that, for the sandy soil system, prokaryotic diversity and N availability
were interrelated. 相似文献
992.
993.
In long-term (20-year-long) experiments, the behavior of different soils under natural conditions different from their usual functioning conditions were analyzed. From soils under natural conditions, organic and mineral substances were partly leached or accumulated under the influence of introduced mixed fir, cedar, and birch falloff. During the time of the experiment, the humus composition distinctly changed. The leached chernozem turned out to be the most stable object; the loamy rock was the least stable one. In the latter, humus was notably accumulated. The intensity of the substance flux through the soils already began to change in 3–5 years, but only after 15 years did some quantitative changes take place. At the same time, the trends of the changes depended on the genesis and initial properties of the soils. The composition of the organic substances in the lysimetric water was related to the soil nature, and, during 20 years, it essentially did not change. 相似文献
994.
Traugott J. Scheytt Petra Mersmann Elzbieta Rejman-Rasinski Anja These 《Journal of Soils and Sediments》2007,7(2):75-84
Background, Aim and Scope
One of the first occurrences of pharmaceutically active compounds in groundwater was reported from the sewage irrigation farms
south of Berlin. At these sewage irrigation farms treated sewage effluent passed the soil and unsaturated zone before reaching
the aquifer. Clofibric acid was detected in pore water from soils of those sewage irrigation farms in concentrations between
65 ng/L and 1430 ng/L. The aim of this study was to investigate the transport behavior of regularly detected clofibric acid,
diclofenac, ibuprofen, and propyphenazone under conditions comparable to those at the sewage irrigation farms in a multiple
compound sand column laboratory experiment.
Materials and Methods
Sediment column experiments were conducted to study the transport of pharmaceuticals in the unsaturated zone. The migration
was measured in fine to medium grained sand and leaching solution containing 1 mg/L of pharmaceutically active compounds and
61 mg/L of the tracer lithium chloride (LiCl). For the analysis of the pharmaceutical compounds the water samples were adjusted
to a pH value of 2 and then extracted by solid-phase extraction (SPE). Before extraction, the samples were spiked with a surrogate
standard for analytical quality control. The sample extracts were analyzed by capillary gas chromatography-mass spectrometry
(GC-MS) with selected ion monitoring (SIM). Depending on the sample volume (100 to 200 mL) and the matrix, the limits of detection
were between 1 and 10 ng/L, and the limits of quantitation were between 5 and 25 ng/L. Analysis for calcium, magnesium and
lithium were carried out using a 'Trace Scan' ICP-AES from Thermo Jarrel Ash. Sodium, potassium, iron and manganese were analyzed
using a Philips PU 9400 flame AAS. Analysis of anions was performed on a Dionex ion chromatograph DX 120.
Results
At the sewage irrigation farms the average concentrations of clofibric acid in the unsaturated zone declined from higher values
near ground surface (480 ng/L) to lower values near the groundwater table (65 ng/L). From the pharmaceuticals analyzed only
clofibric acid, primidone and propyphenazone could be analyzed in the first (upper) aquifer at the sewage irrigation farms.
All other pharmaceuticals could neither be detected in the first aquifer nor in the deeper aquifers. Breakthrough curves from
soil column experiments revealed no transformation and no retardation for clofibric acid, whereas transformation of diclofenac
was so high (79%) that no retardation factor could be calculated. Ibuprofen was significantly transformed (37%), transformation
of propyphenazone (17%) was quite low and retardation (Rf = 2.05) was in the range of previously conducted column experiments.
Discussion
The results confirm previously conducted experiments with clofibric acid where this compound was identified as highly mobile
and persistent. The results that diclofenac and ibuprofen are significantly transformed where unexpected as other studies
exhibited much lower transformation under saturated conditions at least for diclofenac. However, lower pH values and higher
oxygen contents in the unsaturated zone compared to the aquifer may explain this observed high transformation of these compounds
at the column experiments.
Conclusions
We conclude that irrigation with sewage effluent containing the compounds used in our experiments will lead to an input into
groundwater of clofibric acid, whereas diclofenac and ibuprofen will most likely be transformed during the passage. Propyphenazone
will be retarded but will most likely occur in groundwater. These results from the column experiments coincide very well with
the occurrence of the pharmaceuticals clofibric acid, primidone, and propyphenazone in the first aquifer.
Recommendations and Perspective :
The results underline the need to study the sorption of pharmaceuticals on various materials. e.g. organic matter, surfaces
at pH values occurring in the unsaturated zone. Future field studies will also include the investigation of desorption behavior
in the unsaturated zone. 相似文献
995.
Considerable proportions of coastal saline tidelands in China have been reclaimed for agricultural land uses in the past 30
years. This study aims to investigate the potential utility of laboratory hyperspectral data for evaluating the reclamation
levels of those saline lands. A coastal region of Shangyu City (Zhejiang Province) was used as the study area, which was then
grouped into four subzones according to the reclamation history. Soil samples were collected at each subzone, and they were
characterized by high electrical conductivity and sand content and low organic matter; the longer the saline lands have been
reclaimed, the lower the electrical conductivity and sand content are and the higher the organic matter content is. These
changing trends of the soil chemical and physical properties can be indicated by the laboratory reflectance spectra of the
soil samples. Stepwise discriminant analysis (SDA) was applied to select and identify six salient spectral bands at 488, 530,
670, 880, 1400, and 1900 nm. Using derived discriminant functions, saline lands with different historical years of reclamation
were classified with an overall accuracy of 86.6% in a self-test and 89.3% in a cross validation. Finally, this study suggests
that remotely sensed hyperspectral data serve as promising measures to assess the reclamation levels of coastal saline soil,
as opposed to time-consuming field investigations.
Published in Russian in Pochvovedenie, 2007, No. 10, pp. 1226–1233.
The text was submitted by the authors in English. 相似文献
996.
997.
998.
Identification and characterization of foliar polyphenolic composition in sweetpotato (Ipomoea batatas L.) genotypes 总被引:1,自引:0,他引:1
Islam MS Yoshimoto M Yahara S Okuno S Ishiguro K Yamakawa O 《Journal of agricultural and food chemistry》2002,50(13):3718-3722
Trials over two years were conducted using 1389 sweetpotato (Ipomoea batatas L.) genotypes collected from all over the world to characterize the polyphenolic composition in sweetpotato leaves. Wide variation was observed in relation to their total and individual leaf polyphenolic constituents. In all genotypes studied, the total polyphenol contents of sweetpotato leaf ranged from 1.42 to 17.1 g/100 g dry weight. The six different polyphenolic compounds were identified and quantified by NMR, FABMS, and RPHPLC analysis procedures. This is the first report of polyphenolic compositions in sweetpotato leaves. The relative levels of polyphenolic acids in sweetpotato leaves were as follows: 3,5-di-O-caffeoylquinic acid > 4,5-di-O-caffeoylquinic acid > chlorogenic acid (3-O-caffeoylquinic acid) > 3,4-di-O-caffeoylquinic acid > 3,4,5-tri-O-caffeoylquinic acid > caffeic acid. The highest 3,4,5-tri-O-caffeoylquinic acid and 4,5-di-O-caffeoylquinic acid occurred at 221 and 1183.30 mg/100 g dry weight, respectively. 相似文献
999.
Nives Ogrinc Tjaša Kanduč Bor Krajnc Urša Vilhar Primož Simončič Lixin Jin 《Journal of Soils and Sediments》2016,16(2):382-395
Purpose
Soil carbon dynamics were studied at four different forest stands developed on bedrocks with contrasting geology in Slovenia: one plot on magmatic granodiorite bedrock (IG), two plots on carbonate bedrock in the karstic-dinaric area (CC and CD), and one situated on Pleistocene coalluvial terraces (FGS).Materials and methods
Throughfall (TF) and soil water were collected monthly at each location from June to November during 2005–2007. In soil water, the following parameters were determined: T, pH, total alkalinity, concentrations of Ca2+ and Mg2+, dissolved organic carbon (DOC), and Cl? as well as δ13CDIC. On the other hand, in TF, only the Cl? content was measured. Soil and plant samples were also collected at forest stands, and stable isotope measurements were performed in soil and plant organic carbon and total nitrogen and in carbonate rocks. The obtained data were used to calculate the dissolved inorganic carbon (DIC) and DOC fluxes. Statistic analyses were carried out to compare sites of different lithologies, at different spatial and temporal scales.Results and discussion
Decomposition of soil organic matter (SOM) controlled by the climate can explain the 13C and 15?N enrichment in SOM at CC, CD, and FGS, while the soil microbial biomass makes an important contribution to the SOM at IG. The loss of DOC at a soil depth of 5 cm was estimated at 1 mol m?2 year?1 and shows no significant differences among the study sites. The DOC fluxes were mainly controlled by physical factors, most notably sorption dynamics, and microbial–DOC relationships. The pH and pCO2 of the soil solution controlled the DIC fluxes according to carbonate equilibrium reactions. An increased exchange between DIC and atmospheric air was observed for samples from non-carbonate subsoils (IG and FGS). In addition, higher δ13CDIC values up to ?19.4?‰ in the shallow soil water were recorded during the summer as a consequence of isotopic fractionation induced by molecular diffusion of soil CO2. The δ13CDIC values also suggest that half of the DIC derives from soil CO2 indicating that 2 to 5 mol m?2 year?1 of carbon is lost in the form of dissolved inorganic carbon at CC and CD after carbonate dissolution.Conclusions
Major difference in soil carbon dynamics between the four forest ecosystems is a result of the combined influence of bedrock geology, soil texture, and the sources of SOM. Water flux was a critical parameter in quantifying carbon depletion rates in dissolved organic and inorganic carbon forms.1000.
Samuel Raj Babu Arulmani Vimalan Jayaraj Solomon RobinsonDavid Jebakumar 《Journal of Soils and Sediments》2016,16(3):831-841