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Bacteria communities and enzyme activities of PAHs polluted soils

Bacteria communities and enzyme activities of PAHs polluted soils
Bacteria communities and enzyme activities of PAHs polluted soils

Bacterial communities and enzyme activities of

PAHs polluted soils

V.Andreoni a,*,L.Cavalca a ,M.A.Rao b ,G.Nocerino b ,S.Bernasconi c ,E.Dell ?Amico a ,M.Colombo a ,L.Gianfreda

b

a

Dipartimento di Scienze e Tecnologie Alimentari e Microbiologiche,Universita

`degli Studi,Via Celoria 2,20133Milano,Italy

b

Dipartimento di Scienze del Suolo,della Pianta e dell’Ambiente,Universita

`di Napoli Federico II,Via Universita

`100,80055Portici,Napoli,Italy c

Dipartimento di Chimica Organica e Industriale,Universita

`degli Studi,Via Venezian 21,20133Milano,Italy Received 11July 2003;received in revised form 1June 2004;accepted 10June 2004

Abstract

Three soils (i.e.a Belgian soil,B-BT,a German soil,G,and an Italian agricultural soil,I-BT)with di?erent prop-erties and hydrocarbon-pollution history with regard to their potential to degrade phenanthrene were investigated.A

chemical and microbiological evaluation of soils was done using measurements of routine chemical properties,bacterial counts and several enzyme activities.The three soils showed di?erent levels of polycyclic aromatic hydrocarbons (PAHs),being their contamination strictly associated to their pollution history.High values of enzyme activities and culturable heterotrophic bacteria were detected in the soil with no or negligible presence of organic pollutants.Genetic diversity of soil samples and enrichment cultures was measured as bands on denaturing gradient gel electrophoresis (DGGE)of ampli?ed 16S rDNA sequences from the soil and enrichment community DNAs.When analysed by Shan-non index (H 0),the highest genetic biodiversity (H 0=2.87)was found in the Belgian soil B-BT with a medium-term exposition to PAHs and the poorest biodiversity (H 0=0.85)in the German soil with a long-term exposition to alkanes and PAHs and where absence,or lower levels of enzyme activities were measured.For the Italian agricultural soil I-BT,containing negligible amounts of organic pollutants but the highest Cu content,a Shannon index =2.13was found.The enrichment of four mixed cultures capable of degrading solid phenanthrene in batch liquid systems was also studied.Phenanthrene degradation rates in batch systems were culture-dependent,and simple (one-slope)and complex (two-slope)kinetic behaviours were observed.The presence of common bands of microbial species in the cultures and in the native soil DNA indicated that those strains could be potential in situ phenanthrene degraders.Consistent with this assumption are the decrease of PAH and phenanthrene contents of Belgian soil B-BT and the isolation of phenanth-rene-degrading bacteria.

From the fastest phenanthrene-degrading culture C B-BT ,representative strains were identi?ed as Achromobacter xylosoxidans (100%),Methylobacterium sp.(99%),Rhizobium galegae (99%),Rhodococcus aetherovorans (100%),Ste-notrophomonas acidaminiphila (100%),Alcaligenes sp.(99%)and Aquamicrobium de?uvium (100%).DGGE-pro?les of culture C B-BT showed bands attributable to Rhodococcus ,Achromobacter ,Methylobacterium rhizobium ,Alcaligenes and Aquamicrobium .

0045-6535/$-see front matter ó2004Elsevier Ltd.All rights reserved.doi:10.1016/j.chemosphere.2004.06.013

*

Corresponding author.Tel.:+39250316724;fax:+39250316694.E-mail address:vincenza.andreoni@unimi.it (V.Andreoni).

Chemosphere 57(2004)

401–412

https://www.doczj.com/doc/075067500.html,/locate/chemosphere

The isolation of Rhodococcus aetherovorans and Methylobacterium sp.can be consistent with the hypothesis that dif-ferent phenanthrene-degrading strategies,cell surface properties,or the presence of xenobiotic-speci?c membrane car-riers could play a role in the uptake/degradation of solid phenanthrene.

ó2004Elsevier Ltd.All rights reserved.

Keywords:Soil chemical/enzymatic characteristics;DGGE;Bacterial diversity;Phenanthrene consumption;Batch liquid systems

1.Introduction

Polycyclic aromatic hydrocarbons(PAHs)are wide-spread in nature(i.e.soil,water and sediments)because of several polluting anthropogenic activities(Samanta et al.,2002).They have been recognised as a potential health risk due to their intrinsic chemical stability,high recalcitrance to di?erent types of degradation and high toxicity to living organisms(Alexander,1999).

PAHs present in soil may exhibit a toxic activity to-wards di?erent plants,microorganisms and inverte-brates.Microorganisms,being in intimate contact with the soil environment,are considered to be the best indi-cators of soil pollution.In general,they are very sensi-tive to low concentrations of contaminants and rapidly response to soil perturbation.An alteration of their activity and diversity may result,and in turn it will re-?ect in a reduced soil quality(Schloter et al.,2003).Soil enzyme activities are the driving force behind all the bio-chemical transformations occurring in soil.Their evalu-ation may provide useful information on soil microbial activity and be helpful to establish e?ects of soil speci?c environmental conditions(Dick et al.,1996).

Numerous research e?orts are being dedicated to the search of proper remediation technologies to remove as much as possible contaminants from the environment or to transform them into less toxic compounds.Bioreme-diation appears to be an appealing technology to ap-proach the recovery of PAH-polluted sites(Harayama, 1997).Several microorganisms are capable to mineralise a large variety of PAHs and/or to break down them to their less-toxic metabolites(Cerniglia,1992).The very low water-solubility of PAHs and the slow mass-transfer rates from solid phase may limit their availability to microorganisms,thus hindering natural attenuation microbial processes.However,some bacteria degrade sorbed PHAs at di?erent rates,indicating organism-spe-ci?c bioavailability(Grosser et al.,2000).

Bioremediation of PAH contaminated sites rely either on the presence of autochthonous degrading bac-teria which capabilities might be stimulated in situ (Margesin and Schinner,1997),or on the inoculation of selected microorganisms with desired catabolic traits in bioaugmentation techniques(Straube et al.,1999). When microorganisms are added to speed up degrada-tion in contaminated environments,the duration assess-ment and biological process e?ciency depend on the evolution of bacterial communities in terms of composi-tion and catabolic activity.Denaturing gradient gel electrophoresis(DGGE)analysis of16S rRNA genes represents a powerful tool to study the bacterial commu-nity structures in complex environments as well as in enrichment cultures(Muyzer and Smalla,1998).How-ever,the combination of both culture-independent and culture-dependent techniques might provide useful and complementary information on the structure of micro-bial communities.

Soils with di?erent pollution history were preliminary characterized in terms of their chemical properties,enzy-matic activity and culturable heterotrophic bacteria.Site characterization is a pre-requisite when dealing with any remediation approach of a polluted site(Smith and Mason,1999).Indeed,chemical and biochemical proper-ties may assist in the analysis of the ability for the soil to be recovered(Margesin et al.,2000).Moreover,the enrichment and selection of bacterial phenanthrene-degrading cultures,capable of degrading solid phenanth-rene in batch liquid systems were performed.The kinetics of phenanthrene disappearance by enriched cultures,the comparison of their degradation rates and their species composition were also investigated,as assessed by DGGE analysis of PCR-ampli?ed16S rDNA gene fragments. The enrichment of such cultures is a necessary step to obtain microorganisms with the desired catabolic traits, usable in the bioaugmentation of polluted soils.

2.Materials and methods

2.1.Chemicals

Phenanthrene was at>96%purity(Sigma Aldrich, Germany).Solvents at99.9%purity and all the other chemicals,reagent grade were supplied by Analar, BDH Ltd.,(Germany),unless otherwise stated.

2.2.Soil description and sampling

Three soils having a di?erent pollution history were https://www.doczj.com/doc/075067500.html,ly:

(1)A German soil,G,polluted by a long-term exposi-

tion(>50years)to alkanes and PAHs,leading to the formation of a typical light non-aqueous phase

402V.Andreoni et al./Chemosphere57(2004)401–412

liquid(LNAPL)contamination(Saccomandi and Gianfreda,2001).The soil is from Turingia(Ger-many)and its pollution is dated back to II World War.The site is still heavily contaminated because no remediation actions were implemented on it. (2)An Italian agricultural soil,I-BT,from the North

of Italy,with no or negligible presence of pol-lutants.

(3)A Belgian soil,B-BT,from a?uvial canal of Bruxe-

lles(Belgium),characterised by a medium-term(<3 years)exposition to PAHs.The soil was subjected to an accidental pollution event that caused a spread distribution of PAHs on its surface.The soil was sampled after3years from the pollution event.

Italian and Belgian soil samples were taken random by ram-drilling at a depth of5–15cm.German soil was drawn from within the LNAPL phase,immediately above the water table(at a depth ranging from5.5to7.6m below soil surface).Soil samples were packed on-site into sealed polythene bags,and transported to the labo-ratory,stored dark and cooled(4°C).Samples were homogenised,sieved to<0.2mm and stored at4°C until used.

Investigations were performed also on Italian(I-AT) and Belgian(B-AT)soils after bioremediation pilot experiments.Soils were treated aerobically in a bioreac-tor for5months;the experimental procedure adopted and the obtained results are under a patent.Unfortu-nately,no further information was provided by the site?s owner.German soil was not treated because previous laboratory investigations demonstrated that any e?ort to bioremediate it was unsuccessful(Saccomandi and Gianfreda,2001).

2.3.Determination of chemical and microbiological properties

The soils were characterized with respect to both phys-ical and chemical as well as microbiological properties.In particular,a set of enzyme activities(e.g.dehydrogenase,?uorescein diacetate hydrolase,arylsulphatase,phospha-tase and urease)and culturable heterotrophic bacterial cell number were determined.Molecular biodiversity of total bacterial populations was also analysed,according to methods described below(Section2.6).

Chemical and physical analyses were performed on air-dried and sieved(<2mm)samples according to standard techniques(Methods of Soil Chemical Analy-sis,1996).Soil organic C was determined by the method of dichromate oxidation,pH was measured by glass electrode in1:2.5H2O suspensions,total N was meas-ured by the standard Kjeldahl method.Particle size dis-tribution was assessed by the pipette-method.Overall content of PAHs and alkanes of German soil was deter-mined according to Saccomandi and Gianfreda(2001).Heavy metals were determined by atomic adsorption spectroscopy(AAS)after acid digestion with HF/HNO3.

Enzyme activities were determined on fresh moist soils sieved<2mm.The arylsulphatase(ARYL)and phosphatase(PHO)activities were determined according to Tabatabai and Bremner(1970)and Sannino and Gianfreda(2001),respectively.Speci?c substrates(p-nitrophenyl derivatives)and bu?ers were used for each enzyme.Urease(UR)activity was measured as described by Kandeler and Gerber(1988).Dehydrogenase(DH) assays were performed using soluble tetrazolium salt (TTC)as an arti?cial acceptor(Trevors,1984).The activ-ity of?uorescein diacetate hydrolase(FDAH)was as-sessed as described by Adam and Duncan(2001).A unit(U)of ARYL,DH and PHO enzyme activity was de?ned as the micromoles of substrate transformed at 30°Chà1by1g of dried soil.The FDAH and UR activ-ities were expressed as micrograms of substrate hydro-lysed at30°Chà1by1g of dried soil.Control tests with autoclaved soils were carried out to evaluate the spontaneous or abiotic transformation of substrates.

To enumerate culturable heterotrophic bacteria,10g of each soil sample were suspended in45ml sterilised Na4P2O7(0.2glà1in bidistilled water)in300ml glass bottles for1h on a shaker,in order to separate bacteria from soil particles.One millilitre of supernatant ob-tained after10min sedimentation was then10-fold serial diluted in NaCl9glà1solution.Appropriate dilutions were plated onto10%strength Tryptic Soy Agar med-ium for a total heterotrophic bacterial count;100l lmlà1 cycloheximide were added to the medium to inhibit the growth of eukaryotes.The plates were incubated at 28°C for8days and then counted.

Unless otherwise speci?ed,all results reported are averages of triplicate determinations.

2.4.Enrichment and isolation of phenanthrene-degrading cultures

Freshly prepared-phenanthrene stock solution in ace-tone(20mgmlà1)was added to500ml glass bottles.The acetone was allowed to evaporate before adding100ml of autoclaved M9mineral salt medium(Kunz and Chapman,1981)to have a?nal concentration of 200mg là1phenanthrene.Then10g of soil samples were added to a series of bottles.The bottles were te?on-stop-pered and incubated in the dark at25°C with agitation on a reciprocal shaker at96rpm for3weeks.Periodi-cally(3weeks)10ml aliquots of grown cultures were transferred into fresh medium under the same condi-tions.

Di?erent bacteria were isolated from the enrichment cultures.The isolates were grown on M9liquid medium containing100mglà1phenanthrene.Pure cultures were identi?ed by16S rDNA gene nucleotide sequence ana-lysis according to the method below described.

V.Andreoni et al./Chemosphere57(2004)401–412403

2.5.Measurements of phenanthrene utilisation rates

The mixed cultures were grown at25°C with shaking in500ml bottles containing100ml M9mineral medium supplemented with200mglà1phenanthrene.Four bot-tles for each culture were prepared.At each sampling time the concentration of phenanthrene was determined on duplicate sacri?cial bottles and the other two bottles were utilised to perform protein content analysis(Brad-ford,1976)and to extract total DNA(see below).Two bottle-controls(without bacteria)were run in parallel to account for the abiotic loss of phenanthrene.

The extraction and quanti?cation of phenanthrene was determined as follows.Culture broths were ex-tracted three times with50ml CH2Cl2;the organic layers were collected,dried with Na2SO4,?ltered and the sol-vent was removed under reduced pressure.The residue was solved in2ml of ethyl acetate and4ml of a solution of dodecanol in ethyl acetate(5mgmlà1)were added as internal standard for gas chromatographic analyses.The aqueous phase was acidi?ed by conc.HCl(pH2)and ex-tracted three times with50ml ethyl acetate;the organic layers were collected and processed as before described.

Gas-chromatographic analyses were carried out using a DANI1000Gas-chromatograph,equipped with a FID detector(hydrogen0.9bar,air1.0bar and nitro-gen1.0bar)and a fused silica capillary column WCOT-CP-SIL8CB Chrompack(25m·0.32mm ID),carrier helium(0.8bar),and injection temperature300°C, detection300°C,initial oven temperature140°C (3min),temperature increase10°C minà1,?nal iso-therm250°C,injection volume2l l.The dodecanol R t was6.9min and the phenanthrene R t was11.3min. Detector signal output was monitored by computer and all chromatograms and data were generated and processed by Dani Data Station version1.7software.

2.6.Molecular methods

DNA was extracted from soil samples,enrichment cultures and isolated strains.Soil DNA and enrichment culture DNA were extracted by a bead-beating method (MOBIO,USA)and by BIO101method(Resnova, Italy),respectively,according to the manufacturer instructions.According to Cavalca et al.(2002),protein-ase K(1mgmlà1)was used to extract DNA from strains.

PCR ampli?cation of the16S rDNA was performed on the extracted DNA,by using eubacterial universal primers P27f and P1495r referred to E.coli nucleotide se-quence of16S rDNA gene(Cavalca et al.,2002).Nested PCR reaction for V3ampli?cation was carried out according to Muyzer and Smalla(1998).V3PCR prod-ucts from soil,enrichment culture and bacterial isolates DNAs were characterized by a DGGE run on a vertical acrylamide gel in a DCODE Universal Mutation Detec-tion System(Biorad).DGGE was performed with8% (wt/vol)polyacrylamide gels in TAE bu?er(20mM Tris acetate pH7.5,10mM sodium acetate,0.5mM Na2-EDTA)with a linear chemical gradient ranging from 35%to65%.Denaturant solutions were prepared by mix-ing the appropriate volumes of two0–100%denaturant stock solutions(7M urea,and40%vol/vol formamide (Amersham Biosciences,Swedan).Gels were run at a constant voltage of70V for16h at55°C.Gels were stained in a0.5mg là1ethidium bromide solution and documented with GelDoc System(Biorad).Bands of interest were excised from DGGE using an UV transillu-minator.The excised bands were suspended into200l of PCR water,reampli?ed and sequenced.The nucleotide sequences of16S rDNA of the resulting amplicons and of isolates were determined according to the Perkin El-mer ABI Prism protocol(Applied Biosystems,USA). Primers used in the PCR reaction for sequencing prod-ucts were the same of those in normal16S rDNA PCR reactions.The forward and reverse samples were run on an Applied Biosystems310A sequence analyser.The sequences were compared with similar sequences of refer-ence organisms deposited in public domain databases.

DGGE analyses were performed to compare the bac-terial community structures of soils and enrichment cul-tures.Although the technique could be associated with a variety of PCR biases(Wintzingerode et al.,1997;Fro-min et al.,2002),it provides comprehensive information on the global patterns of microbial diversity(Torsvik and Overas,2002).However,to minimize biases,DGGE analyses were performed on samples treated using iden-tical methods in which DNA extraction and ampli?ca-tion biases are supposed to occur homogeneously.

Shannon index(H0)(Magurran,1988)was used to evaluate the biodiversity of both soils and enrichment cultures,and Sorensen index(S)(Magurran,1988)to evaluate the similarity within soils(native vs.treated soil)and within the deriving cultures.

The Shannon index of soils was calculated on the ba-sis of the number and intensity of bands present on DGGE samples,run on the same gel,as follows: H0?à

P

P i log P i,where P i is the importance probabil-ity of the bands in a gel lane.P i was calculated as fol-lows:P i=n i/N,where n i is the band intensity for each individual band and N is the sum of intensities of bands in a lane.Statistical comparison of di?erent DGGE pro-?les was done with the GelDoc software package.This latter assumes that the population size is proportional to the thickness of bands.Gel analysis included conver-sion of the scanned gel image and normalization in order to correct shift within or between gels,so that bands or peaks of the same molecular size have the same physical position relative to a standard.Once all banding pro?les were in a standardized analysis format,each band could be described by its position on the gel and by its relative intensity.

404V.Andreoni et al./Chemosphere57(2004)401–412

3.Results and discussion

3.1.Physico-chemical and microbiological properties of

soils

The chemical and physical properties of a soil as well as the evaluation of its pollution degree may help to esti-mate the impact of pollutants on the quality of soil un-der investigation,if they are complemented with the measurement of biological properties (Margesin et al.,2000).

Tables 1and 2summarise the physical and chemical properties of investigated soils and the amounts of both organic and inorganic pollutants.

The moderate-high amounts of carbonate and the pH values (measured in H 2O),ranging from 2.68to 5.36and from 6.73to 8.19,respectively,indicate a sub-to moder-ate-alkaline character of soils (Table 1).At the measured pH range soil microbial growth and its activity are usu-ally favoured.As discussed by Smith and Doran (1996),soil pH can provide valuable information on the availa-bility and toxicity of several elements,including Fe,Al,Mn,Cu,Cd and others to plants and microorganisms.German and Italian soils showed comparable amounts of clay,silt and sand fractions (Table 1)whereas Belgian soil had a very low amount of both clay ($7%)and silt ($8%)and a predominant presence of sand (>80%as total of coarse and ?ne fractions).According to USDA classi?cation (Soil Survey Sta?,1993),German and Italian soils can be classi?ed sandy clay loam soils while Belgian is a typically loamy sand soil.

In Belgian and mainly in German soil before treat-ment (B-BT and G)total organic C values,and conse-quently organic matter contents,were very high,being in?uenced by organic pollutant contamination.Thus,their values did not represent natural,endogenous soil organic matter levels,possibly present in the soil in the absence of any contamination.Considering the low amounts of N measured in both soils,the C/N ratios (11.5and 26.3for B-BT and Gsoils,respectively)were higher than those normally found in unpolluted soils.When hydrocarbon-polluted soils are considered,much higher C/N ratios,ranging from a minimum value of 9:1to a maximum of 200:1,are,however,needed to ob-tain a consistent microbial growth and resulting hydro-carbon degradation (Bewley,1996).

The physical and chemical properties of Belgian and Italian soils were also measured after the bioremediation treatment (Table 1).As expected,no signi?cant varia-tions of clay,silt and sand fractions were noted.The 2-fold higher amounts of both N and available K meas-ured in B-AT are likely the result of nutrient supply dur-ing the biological treatment.

According to the current European Union regulation (Commission of the European Communities,1986)

T a b l e 1P h y s i c a l –c h e m i c a l p r o p e r t i e s o f s t u d y s o i l s

S o i l

p H (H 2O )

C a C O 3

(%)

M o i s t u r e (%)

C l a y (%)

S i l t (%)

C o a r s e s a n d (%)F i n e s a n d (%)

O .C .(g k g à1)O .M .(g k g à1)

T o t a l N (g k g à1)

C /N

P -O l s e n (m g k g à1)

A v a i l a b l e K (m g k g à1)

B e f o r e t r e a t m e n t G e r m a n 6.73a *

3.07a

13.0a 24.7a 15.0a 22.0a 38.3a 11.1a 19.1a 0.422a 26.3a T r a c e

n d

(G )(±0.23)a

(±0.15)(±0.90)(±1.5)(±0.97)(±0.99)(±1.0)(±1.50)(±2.20)(±0.09)(±3.45)I t a l i a n 7.67b 3.93a 14.5a 22.5a 24.5b 19.5b 33.4b 7.70b 13.3b 2.20b 3.5b 33.7a 337b (I -B T )(±0.56)(±0.21)(±1.10)(±2.0)(±2.4)(±1.30)(±2.10)(±1.20)(±1.90)(±0.50)(±0.45)(±4.50)(±17.8)B e l g i a n 8.19b 2.93a 11.0a 6.94b 7.75c 40.0c 45.3c 8.2b 14.1b 0.71c 11.5c 15.0b 224c (B -B T )(±1.10)

(±0.09)

(±0.85)(±0.54)

(±0.65)

(±3.20)(±3.60)

(±1.60)

(±2.20)

(±0.09)

(±1.20)

(±1.50)

(±13.4)

A f t e r t r e a t m e n t I t a l i a n 7.73b 5.36b 18.5b 21.6a 23.9b 18.9a 35.6b 7.9b 13.6b 2.85d 2.8b 30.5a 574d (I -A T )(±0.61)(±0.35)(±1.20)(±2.0)(±2.70)(±1.40)(±3.10)(±1.50)(±2.10)(+0.60)(±0.38)(±3.90)(±20.7)

B e l g i a n 8.17b 2.68a 11.0a 6.90b 8.58c 38.6c 45.9c 8.20b 14.1b 1.40e 5.8d 20.2c 495e (B -A T )(±0.60)

(±0.10)(±0.91)(±0.54)(±0.74)(±1.93)(±2.30)

(±0.90)(±1.50)

(±0.80)(±0.40)

(±0.80)

(±18.5)*

F o r e a c h v a r i a b l e d i ?e r e n t l e t t e r s a l o n g s i d e c o l u m n s r e f e r t o s i g n i ?c a n t d i ?e r e n c e s (P (0.05).a V a l u e s i n p a r e n t h e s e s r e p r e s e n t s t a n d a r d d e v i a t i o n .

V.Andreoni et al./Chemosphere 57(2004)401–412405

referring to agricultural soils,investigated soils showed levels of heavy metals all below the maximum permitted concentrations,except for copper in Italian soil that was about twice the safe limit(150mgkgà1soil).

A di?erent situation holds when organic pollutants are considered.German soil resulted heavily polluted by high concentrations of alkanes and PAHs.BTEX and phenols were also detected(data not shown),thus con?rming the presence of a LNAPL widespread pollu-tion(Saccomandi and Gianfreda,2001).In contrast, these pollutants were not detected in Italian soils. Belgian soil presented a detectable amount of PAHs (30.8mgkgà1),being phenanthrene relatively the most abundant(Table2).

The activities of?ve enzymes and the heterotrophic bacteria of the investigated soils are reported in Table3. Arylsulphatase and phosphatase release sulfate and phosphate,the main plant and microbial available S and P forms,from various organic sulfate and phos-phate esters(Nannipieri et al.,2002).Urease catalyses the hydrolysis of urea to carbon dioxide and ammo-nium,and it is widely distributed in microorganisms, plants and animals(Nannipieri et al.,2002).Dehydro-genase activity typically occurs in all intact,viable

Table2

Amounts of inorganic and organic pollutants of study soils

Inorganic(mgkgà1)Organic(mgkgà1)

Soil Cu Zn Cr Ni Fe Alkanes PAH Phenanthrene Before treatment

German145a*88.0a14.0a39.0a 6.1a29094a14a

(G)(±8.7)a(±9.4)(±2.7)(±8.2)(±3.6)(±10.1)(±6.4)(±2.6)

Italian301b121b72.4b75.5b40.3b nd nd nd

(I-BT)(±21.5)(±9.6)(±6.5)(±8.5)(±5.4)

Belgian50.2c124b83.9c55.4c39.0b nd30.8b 4.7b

(B-BT)(±5.3)(±7.5)(±5.3)(±6.5)(±5.6)(±3.2)(±0.7)

After treatment

Italian290b265d70.8b85.7b25.9c nd nd nd

(I-AT)(±19.3)(±12.1)(±5.8)(±9.1)(±3.2)

Belgian52.9c329e67.4b65.6d33.4d nd8.9c0.7c

(B-AT)(±8.5)(±17.5)(±6.4)(±7.6)(±2.4)(±0.87)(±0.6)

*For each variable di?erent letters alongside columns refer to signi?cant di?erences(P(0.05).

a Values in parentheses represent standard deviation.

Table3

Enzyme activities and microbial counts of study soils

Soil ARYL

(l molgà1hà1)PHO

(l molgà1hà1)

UR

(l ggà1hà1)

DH

(l ggà1hà1)

FDAH

(l ggà1hà1)

Total

heterotrophs

CFU(gà1)

Before treatment

German nd 4.10a nd18.9a nd 3.9·105a (G)(±0.045)(±2.1)(±4.0·104) Italian0.388a* 2.20b18.4a0.748b186a 4.9·107b

(I-BT)(±0.07)a(±0.31)(±1.7)(±0.03)(±6.45)(±4.0·106) Belgian0.014b0.35c nd nd8.52b 2.3·107c

(B-BT)(±0.003)(±0.21)(±0.91)(±2.0·106) After treatment

Italian0.555c 3.84d18.8a 1.27c197c 3.9·108d

(I-AT)(±0.09)(±0.40)(±1.6)(±0.08)(±6.51)(±5.0·107) Belgian0.265d 2.90b nd0.049d162d 5.8·108e

(B-AT)(±0.02)(±0.1)(±0.01)(±5.56)(±6.0·107) nd=not detected.ARYL=arylsulphatase,PHO=phosphatase,UR=urease,DH=dehydrogenase,FDAH=?uorescein diacetate hydrolase.

*For each variable di?erent letters alongside columns refer to signi?cant di?erences(P(0.05).

a Values in parentheses represent standard deviation.

406V.Andreoni et al./Chemosphere57(2004)401–412

microbial cells.Thus,its measurement is usually related to the presence of viable microorganisms and their oxi-dative capability(Trevors,1984).Fluorescein diacetate hydrolase(FDAH)has been often used as a sensor and functional indicator of soil health(Adam and Dun-can,2001).Being the?uorogenic substrate uptaken by active cells and then transformed by a large arrays of hydrolytic enzymes,the enzyme has been considered a measure of the soil microorganism activity(Killham and Staddon,2002).

Enzyme activities and total heterotrophs,mainly for Belgian and German soils,are in agreement with the re-sults obtained with soils contaminated by similar pollut-ants(Kiss et al.,1998;Margesin et al.,2000).The German soil was the most contaminated compared to Belgian and Italian soils,having the lowest number of heterotrophs(Table3).

After the biological treatment an increase in CFU of only one order of magnitude was measured in both Bel-gian and Italian soils(Table3).As reported by Margesin et al.(2000)total number of heterotrophs of PAHs pol-luted soils did not greatly increase after biological reme-diation actions,whereas the relative amounts of speci?c pollutant-degrading bacteria increased to a detectable extent.

Enzyme activities also con?rmed that the Italian soil showed the highest microbiological activity.All the measured enzymes were present at moderate to high range levels,usually found in agricultural soils(Nannipi-eri et al.,2002).The relatively low dehydrogenase activ-ity measured in this soil(which seems to contradict the high values of both FDAH activity and total microor-ganisms)could be explained by the possible interference exerted by the high Cu content(Table2)on the analytic assay used.Indeed,Cu may reacts abiotically with the triphenylformazan,the end product of DH catalysis, thus resulting in a underestimation of the soil dehydro-genase activity(Chander and Brookes,1991).

Although the in?uence of other factors deriving from natural and anthropogenic events cannot be ruled out (Gianfreda and Bollag,1996),the complete absence and/or the very low enzymatic activities of both German and Belgian soils could be also partly due to the presence of PAHs in soils.As extensively reviewed by Kiss et al. (1998),even moderate levels of hydrocarbon contamina-tion may cause a signi?cant decline of several soil en-zyme activities,showing each enzyme a di?erent sensitivity to the presence of pollutants.Although the interpretation of enzyme activities of soil is complex be-cause both extracellular and intracellular enzyme activi-ties contribute to the overall soil enzyme activity,some hypotheses might be advanced.In soil,non-polar organ-ic compounds,such as hydrocarbons,may likely exert di?erent e?ects on microbiological properties.Hydro-carbons may be toxic to soil microorganisms which may re?ect in a consistent reduced enzymatic activity;and/or they my cover both organic-mineral and cell sur-faces,thus hindering the interaction between enzyme ac-tive sites and soluble substrates with adverse e?ect on enzyme activity expression(Kiss et al.,1998).Moreover, a synergistic negative e?ect on soil enzyme activities ex-erted by the simultaneous presence of heavy metals can-not be ruled out.

After bioremediation,enzyme activities of Italian and Belgian soils increased to a moderate and a more detect-able extent,respectively.

3.2.Biodiversity of soils

In our analysis,the number of DGGE bands was taken as an indication of species in each sample.The rel-ative surface intensity of each DGGE band and the sum of all the surfaces for all bands in a sample were used to estimate species abundance(Fromin et al.,2002;Sekig-uchi et al.,2002).DGGE pro?les of soils are shown in Fig.1.Many DGGE bands were observed in the pro-?les,thus indicating the presence of di?erent bacterial populations and di?erent relative abundance species in soils.As indicated by the values of Shannon indices, contamination of soils appeared to a?ect their genetic diversity:German soil and native Belgian soil B-BT showed the pooresteH0

G

?0:85Tand the highest

eH0

BàBT

?2:87Tbiodiversity,respectively.For the Italian agricultural soil I-BT,containing negligible amounts of organic pollutants but the highest Cu content,a Shan-non index=2.13was found.

After treatment,a loss of bacterial species diversity

occurred in Belgian soil with a H0

BàBT

equal to1.13.Fur-thermore,the bacterial community of the native soil B-BT showed a marked di?erent pattern when compared with its treated B-AT counterpart.Indeed,the S index of similarity was equal to0.18.Only few bands(‘‘a’’and‘‘b’’in Fig.1)were in common between the two soils,indicating the survival of some predominant species.

On the contrary,for Italian soils only negligible dif-ferences in DNA patterns(S=0.56)were evidenced be-tween the native I-BT and its treated I-AT counterpart

eH0

IàAT

?2:14T,indicating that the bioremediation did not substantially change the community structure of the native one.

3.3.Enrichment of phenanthrene-degrading mixed cul-tures and determination of degradation kinetics

The diversity encountered in the bacterial communi-ties of the study soils prompted us to perform enrich-ments on phenanthrene from all soil samples in order to obtain cultures with di?erent potential strategies to degrade phenanthrene.

Attempts to enrich phenanthrene degrading bacteria from the German soil were unsuccessful(Saccomandi

V.Andreoni et al./Chemosphere57(2004)401–412407

and Gianfreda,2001).The presence of highly bound res-idues in the old-contaminated German soil could have represented a constraint in phenanthrene bioavailability to bacteria thus impairing the possibility to isolate degrading microorganisms.

Four mixed bacterial cultures,named C B-BT and C B-AT,and C I-BT and C I-AT were instead selected from the Belgian and Italian soils before and after the biolog-ical treatment,respectively.

All cultures enriched from Belgian and Italian soils grew on phenanthrene when added as sole C and energy source and turbidity of culture broths increased during incubation.

Fig.2shows the disappearance of200mglà1crystal-line phenanthrene and the corresponding protein con-tents within21-d incubation of the selected cultures.A time course analysis of phenanthrene may provide an estimate of?rst order uptake/degradation rate constant according to the following expression:X t=X0eàkt, where X t is the concentration of phenanthrene in mglà1, k is the uptake/degradation constant and t is the time.

When phenanthrene degradation data of Fig.2were reported in a semilog plot,a one-slope behaviour was observed for C B-BT and C I-AT cultures,while a typical two-slope occurred for C B-AT and C I-BT,suggesting a more complex kinetics of phenanthrene degradation by these cultures(data not shown).This could imply that for culture C B-BT and C I-AT the whole phenanthrene degradation process is dominated by a single,straight-forward key step,whereas for cultures C B-AT and C I-BT a complex mechanism,involving a slower interme-diate step,occurred.

Table4reports the degradation constants calculated by means of a non-linear regression routine applied to phenanthrene degradation data of Fig.2.The?rst step-kinetics occurring for C B-AT and C I-AT,character-ized by low degradation constants,could suggest a slower utilisation of phenanthrene within the?rst8 days.In particular,the very low k1value(0.020dà1)cal-

Fig.1.DGGE analysis of PCR-ampli?ed16S rDNA gene V3fragments from soil samples and from enrichment cultures after six transplants on fresh phenanthrene.Bands were designated as described in the text.G,German soil;B-BT,Belgian soil before treatment;B-AT,Belgian soil after treatment;I-BT,Italian soil before treatment;I-AT,Italian soil after treatment;C B-BT,C B-AT, C I-BT,C I-AT,enrichment cultures from the corresponding soil samples.

408V.Andreoni et al./Chemosphere57(2004)401–412

culated for C B-AT could indicate the presence of a slow phenanthrene mass transfer resulting in a hampered PAH utilisation.By contrast,the mixed culture C B-BT al-most completely utilized200mglà1phenanthrene(more than90%)within10days.Longer times were required for complete degradation by C I-AT and C B-AT(Fig.2 and Table4).All cultures degraded phenanthrene without the appearance of any metabolites in culture broths.

The protein content patterns of culture broths con-?rmed the ability of strains to utilise phenanthrene as the sole C source.The pro?les of protein contents vs. phenanthrene disappearance of cultures C I-AT and C I-BT were the same as C B-BT(data not shown).

C B-AT protein content seems to con?rm that the con-sumption rate by this culture was limited by dissolution dynamics.Indeed,the growth rate of C B-AT,evaluated as protein content(2.33l g mlà1dà1)in the exponential (0–21d)growth phase was lower than that measured for C B-BT(7.78l gmlà1dà1)in the exponential(0–5d) growth phase.The di?erent behaviour of C B-BT com-pared to C B-AT,enriched from the same soil after the biotreatment,could be referred to a di?erent species composition of the cultures(Fig.1).The former con-tained probably bacteria with di?erent PAH-degrading strategies or with di?erent cell surface properties.A bac-terial adhesion to solid phenanthrene and subsequent solubilisation at the level of the cell wall could be hypothesised.Similar mechanisms have been suggested for degradation of solid hydrophobic chemicals(pal-mitic acid)by Pseudomonas strains(Thomas and Alex-ander,1987).

Culture C I-BT,obtained from the Italian agricultural soil I-BT,was for the?rst8days metabolically less ac-tive than culture C B-BT obtained from the Belgian con-taminated soil B-BT.A faster degradation occurred, however,in the last incubation period(k2value for C I-BT higher than k1value for C B-BT,Table4).A dif-ferent phenanthrene-degrading culture was selected from the Italian biotreated soil I-AT and its degrada-tion rate was slower than that of I-BT(Fig.2and Table4).3.4.Biodiversity of enrichment cultures

The DGGE pro?les of the mixed cultures analysed after six21-d-incubation transplants on phenanthrene, when cultures were supposed to be stable and used also for degradation kinetic experiments,are shown in Fig.1. DGGE pro?les of enrichment cultures were less complex than soil pro?les,due to the selective pressure repre-sented by the presence of fresh phenanthrene.

All the cultures showed DGGE pro?les that indi-cated a di?erent bacterial species composition,as evi-denced by the presence of peculiar bands in each culture(Fig.1).Sorensen similarity values calculated from DGGE pro?les revealed that there were signi?cant di?erences in species composition of cultures from each native and treated soil(S=0.33for C B-BT vs.C B-AT and 0.25for C I-BT vs.C I-AT).Some bands were in common among enrichment cultures,indicating the presence of similar bacterial species,such as band‘‘g’’in C B-BT, C B-AT and C I-BT.Other bands were visible in the enrich-ment culture DNA pro?les and in the corresponding soil samples(band‘‘a’’in C B-BT and C B-AT,in B-BT and B-AT,and band‘‘c’’in C I-BT and C I-AT,in I-BT and I-AT).All these bands belong to species that could be relevant in situ phenanthrene degraders and that have been enriched during the transplant procedure.Four bands(‘‘d’’,‘‘e’’,‘‘f’’and‘‘g’’)were in common among DNA pro?les of C B-BT and C B-AT,thus con?rming their presence in the native and treated Belgian soils(Fig.1).

The di?erences encountered in the DGGE pro?les could re?ect the di?erent degradative kinetics of the four cultures.The presence of di?erent species could assure a probable existence of di?erent mechanisms for e?cient assimilation/uptake of soluble or solid phenanthrene.

Colonies with di?erent morphologies were isolated from the fastest degrading culture C B-BT after growth on0.1·tryptic soy broth agar plates.Representative strains of C B-BT,identi?ed on the basis of1200nucleo-tides sequence homologies with entries in GenBank-EMBL databases,belong to:Achromobacter xylosoxidans (100%),Methylobacterium sp.(99%),Alcaligenes sp. (99%),Rhizobium galegae(99%),R.aetherovorans (100%),Aquamicrobium de?uvium(100%)and Stenotro-phomonas acidaminiphila(100%).When these strains were checked for the capability of growing on100mglà1 crystalline phenanthrene as sole C source,the growing strains had di?erent growth behaviour.While R.aether-ovorans produced a di?use turbidity of culture broths (data not shown),Methylobacterium sp.grew in contact with the phenanthrene crystals,as revealed by micro-scopic examination.This implies that the low solubility of phenanthrene was limiting the growth,and the few cells freely present in the culture broth were probably those sloughed o?from the crystal surfaces.

The presence of strains within the culture C B-BT dur-ing the time course of phenanthrene degradation was

Table4

Values of phenanthrene(200mglà1)disappearance constants

calculated for the cultures enriched from the study soils

Culture k1(dà1)k2(dà1)R2

C B-BT0.369–0.95

C B-AT0.0200.2970.99

C I-BT0.1130.5100.99

C I-AT0.076–0.98

k1and k2calculated by a non-linear regression routine

according the equation X t=X0exp(àkt)where X t is the con-

centration of phenanthrene in mglà1,k is the uptake or trans-

formation constant and t is time.

V.Andreoni et al./Chemosphere57(2004)401–412409

followed by DGGE analysis.During the degradation process,no change was evidenced in the bacterial com-ponents of C B-BT (Fig.3)but some bands increased their relative intensity.

C B-BT bands were correlated to the isolated strain bands (Fig.3)on the basis of their electrophoretic mobility.Theoretically,bands at the same position in the electrophoresis pattern contain DNA fragments with identical sequences.Band ‘‘h’’had the same electropho-retic mobility of R.aetherovorans ,band ‘‘l’’the same of R.galegae and Aquamicrobium de?uvium ,band ‘‘m’’the same of Methylobacterium sp.,band ‘‘n’’the same of Alcaligenes sp.and of one of the two bands of A.xylos-oxidans and band ‘‘p’’the same of the other band of A.xylosoxidans .Bands corresponding to R.aetherovorans and A.xylosoxidans increased their relative intensity during phenanthrene degradation suggesting that these strains represent active members of the culture and are likely involved directly or indirectly in the utilization of phenanthrene as C and energy sources.

The overlapping of ampli?ed PCR products cannot con?rm that sequences of these isolates are identical to the sequences of corresponding DGGE enrichment cul-ture bands.

Band corresponding to St.acidaminiphila has never been retrieved in culture C B-BT DGGE pro?les.This could be due either to its low cell number in the culture or to the DNA applied extraction method.Conversely,species corresponding to bands ‘‘a’’and ‘‘g’’in the DGGE pro?les of culture C B-BT were not recovered among isolates,and their sequence types were identi?ed as Pseudomonas and Arthrobacter ,respectively.The ampli?cation of these bands may be due to biases in selective PCR ampli?cation (Heuer and Smalla,1997).The bands corresponding to P.putida and Ralstonia sp.have approximately the same relative intensity dur-ing incubation time,suggesting that these species do not increase during phenanthrene degradation.

4.Conclusions

The results,here presented,all indicate that soils highly contaminated by hydrocarbons displayed di?er-ent microbiological properties.In particular the higher/the lower the pollutant content,the smaller/the greater are the activities of some enzymes related to nutrient cycling and the viable bacterial cell numbers.The di?er-ent microbiological properties of the soils probably re?ect the di?erent bacterial diversity as assessed by DGGE pro?les of the 16S rDNA genes.

Phenanthrene-degrading mixed cultures were en-riched from all soils except the old heavily contaminated German soil.When tested in liquid batch systems using solid phenanthrene as C and energy source,cultures showed di?erent kinetic behaviours probably because of a di?erent species composition,as evidenced by DGGE 16S rDNA pro?les.The presence of di?erent species could indicate a probable existence of di?erent mechanisms for e?cient assimilation/uptake of soluble or solid phenanthrene,as observed for C B-BT culture that contained more than one phenanthrene-degrading bacterium.The simultaneous presence in the culture of Rhodococcus and Methylobacterium strains might be ex-plained with the capability to use phenanthrene under di?erent conditions such as dissolved,solid associated,and perhaps surfactant-associated,according to di?erent substrate-degrading strategies.C B-BT culture also con-tained bacteria that do not use phenanthrene,suggesting that the phenanthrene-degraders themselves may be associated with bacteria using metabolites of phenanth-rene.The presence of some DGGE bands with the same electrophoretic mobility and the presence of degrading strains belonging to the same species in all the enrich-ments are indicative of their degradative role in the cul-tures.The isolation of bacteria from B-BT soil,that are able to grow on phenanthrene,is consistent with the ob-served decrease of PAH and phenanthrene contents of soil after the biotreatment and suggests that aerobic phenanthrene biodegradation was occurred.The

?nding

Fig. 3.DGGE analysis of V3fragments obtained from uncharacterized bacterial culture C B-BT and bacterial isolates from the https://www.doczj.com/doc/075067500.html,nes T 0(P )to T 8(P )show the pro?les obtained from C B-BT after 0,2,4and 8day growth in presence of phenanthrene;lane V 3MIX contains the separation pattern of a mixture of fragments of seven isolates,i.e.,Alcaligens sp.(lane 1);Rhizobium galegae (lane 2);Methylobacterium sp.(lane 3);Stenotrophomonas acidaminiphila (lane 4);Aquamicrobium de?uvium (lane 5);Achromobacter xylosoxidans (lane 6)and R.aetherovorans (lane 7).

410V.Andreoni et al./Chemosphere 57(2004)401–412

that a number of bacteria identi?ed in culture C B-BT de-grade phenanthrene supports this assumption.The iso-lation of R.aetherovorans and Methylobacterium sp. can be consistent with the hypothesis that di?erent phen-anthrene-degraders inhabiting soils and enrichment cul-tures may be adapted to di?erent phenanthrene bioavailabilities.The use of these species in microcosm bioaugmentation trials could help in evaluating their in situ catabolic behaviour to degrade phenanthrene in highly polluted soils.

Acknowledgments

This research was supported by Ministero dell?Uni-versita′e della Ricerca,Italy,Programmi di Interesse Nazionale PRIN2002-2003.Dr.Fornaro E.of ENVIR-OREM,Lugane,Switzerland is thanked for the kind supply of Belgian and Italian soil samples and for the determination of their phenanthrene content.DiSSPA Contribution no.049.

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三五计划内使中医类别执业医师(含执业助理医师)占执业医师比例大于60%;中药专业技术人员占药学专业技术人员的比例大于60%;护理人员系统接受中医药知识和技能岗位培训的比例不低于70%。每个临床科室执业医师中至少有60%中医类别执业医师(麻醉科、口腔科除外)。 (二)定期组织医、护、药人员进行中医基础理论和基本技能培训,并熟练掌握各种技能。每年要求我院全体护理、药学人员系统主动学习中医中药理论基础知识,提高中医护理工作技能。 (三)结合我院实际,要求现有领导班子成员,认真学习中医知识,参加中医管理培训教材。医院主要负责人、业务管理领导和医务、护理、药剂、教学、科研部门的主要负责人经过中医药政策、中医药知识和管理知识的系统培训。对参加中医中药学历提高学习的人员,给予一定的补助和奖励。 (四)临床科室负责人中有计划调整充实中医类别执业医师

治妇科病最常用的7种养生中药

治妇科病最常用的7种养生中药 治妇科病最常用的7种养生中药。女人天生爱美,然而受妇科病的困扰,严重了影响了美丽与健康。这是因为妇科病不仅损害身体健康,还会影响容颜,使脸上长痘痘、肌肤暗淡无光等。人们往往采用中药治疗方法。下面介绍治妇科病最常用的7种养生中药。 1、当归:李时珍认为,当归是女人调血的要药。从我国南北朝开始,当归就被视为补血活血珍品。补血调经、活血止痛、泽颜润肤、生肌强体、延年益寿。在保护女性健康方面极其重要。 2、枸杞子:是我国最早记载的一味妇科用药,可滋阴养血,益肝补肾,能明目润肤,乌发养颜。《重庆堂随笔》评价它:“专补心血,非他药所能及。”《中药大辞典》认为它滋肾、润肺,补肝,明目。 3、黄芪:能够增强皮肤营养和皮肤的抗菌能力,防止皮肤老化,促进毛发生长,防止脱发。它含有多种氨基酸及人体必需微量元素和叶酸等,具有全面营养作用。中医认为,它能够补中益气,对气虚血脱、崩带及一切气衰血虚之症有疗效。 4、白芍:《日华子本草》评价它:“治风补涝,主女人一切病,并产后诸疾。”《唐本草》说它“益女子血。”现代中医认为,它能够养血柔肝、缓中止痛,对月经不调,崩漏,带下有效果。 5、珍珠:珍珠历来是名贵的中药材,对皮肤有特殊的滋养保健作用,能保持颜面细腻白嫩,并可促进人体细胞再生,防止衰老,延缓皱纹产生。中医认为,它具有养阴安神、镇心熄风清热、解毒生肌等功效,可治眩晕、耳鸣、烦躁、头痛、失眠、惊悸等病症。 6、芦荟:对女性来说,芦荟是最熟悉不过的美容佳品。中医看来,芦荟能治疗清热、通便、热结便秘、妇女闭经等症。 7、川芎:川芎在唐朝《日华子本草》中有着很高的评价:“治一切风,一切气,一切劳损,一切血,补五劳,行气开郁,活血止痛,对经闭、难产、产后瘀阻块痛等有效。壮筋骨,调众脉,养新血……”《医学启源》:“补血,治血虚头痛。” 以上7种中药都是最常见的药材,在治疗妇科病方面有很好的治病养生疗效。有些中药可以用来泡水喝。女性朋友选择中药时,一定根据自身体质及症状等因素而定。

如何正确煲中药

如何正确煲中药 煲中药就是简单的“3碗水煮成1碗”?非也!最近与朋友讨论起如何煲中药,才发现许多年轻的广州人,虽然一有什么“头晕身热”都会习惯地煲中药喝,但到底怎样煲中药才是正确,往往只是一知半解,道听途说。其实,煲中药,还真是一件有技术含量的事! 煎煮前——— ●清洗 中药材是否需清洗,这是很多人的疑问虽然很多中药饮片看起来表面会有些灰黑,其实在出售前都经过了加工炮制,所以煎煮之前一般无需清洗。如果实在觉得草药有些泥沙,可以用水迅速漂洗一下,但切忌浸洗,以免一些水溶性成分丢失,以及一些细小种子类的药材(如车前子等)被冲走流失。 ●浸泡 清洗步骤不能浸泡中草药,但煎煮之前,却需要有个浸泡药材的过程。 煎煮前用凉水浸泡药材约半小时,可以使水溶性成分析出在汤水中,同时也能增加汤药的浓度。冬天可以用20-30度的温水浸泡,以缩短煎煮时间,但切不可用开水浸泡,以免某些植物细胞中的蛋白质受热凝固,或是部分高分子物质形成胶体,不利于有效成分析出。 浸泡时间不宜超过1小时,特别是在夏天,浸泡时间过长会很容易引起酸败。 煎煮中——— ●用水 传统的“3碗水煮成1碗”,其实不是个科学的标准。因为不同处方的药味多少、药量大小各有不同,不同药材吸水量也有不同。如果真的有人一边煲药,一边不断把药汁倒来倒去,作为煲中药的标准,这样瞎折腾其实也不可能煲出最佳效果的中药。 应以水浸过药材面2-3cm为佳,或者用手轻轻摁住药材,水面刚好漫过手背。而不是机械地用3碗水煮药。通常一些花草类的药物吸水量较大,在浸泡半小时后水位下降,可以另加凉水至标准水位,再开始煎煮。 ●火候 一般的中药应先用武火,煮沸后改为文火。控制火候的意义在于,若火候过强,水分蒸发过快,影响有效成分的析出,亦易焦糊。 但一些治疗外感的中药,可以在煮沸之后不改文火,继续用武火煎煮15分钟左右即可。 ●时间 中药煎煮时间,应根据不同药物和疾病性质、有效成分溶出的难易和用药情况而定。楼步青说,沸腾后再用文火煲药的时间,一般中药,头煎应在20-25分钟,二煎15-20分钟;解表类中药,头煎10-15分钟,二煎10分钟;滋补类中药,头煎应在30-40分钟,二煎25-30分钟。 如果有“大头虾”不慎煎煮时间过长,令药汤太浓,这时可以加些白开水再煮沸,就可以避免有效成分反渗透的问题。 ●复煎 许多老人家习惯于一副中药“返煎”三四次,楼步青说,一般而言,一副中药在煎煮两次后,所含有效成分已大为降低,故以煎煮两遍为佳。但滋补类的中药,可以煎煮三次。而一些药量较大的处方,也可以煎煮三遍。 但需注意的是,如果将头煎与二煎的药液分别服用,这样未能将药效发挥至最佳。应该将头煎与二煎的药液混合,分早晚两次服用。同样,煎煮三遍的药液也相应地改为一天3次服用。 煎煮后——— ●立即滤取 药汤煎煮好,应趁热过滤倒出,不宜久置锅中。否则含胶体过多的药液,随温度下降产生胶凝,难以过滤,

中成药临床应用指导原则(正式版)

中成药临床应用指导原则

目录 前言 (2) 第一部分中成药概述 (3) 一、中成药的剂型 (3) 二、中成药分类 (4) 三、中成药安全性 (5) 第二部分中成药临床应用原则 (6) 一、中成药临床应用基本原则 (6) 二、联合用药原则 (6) 三、孕妇使用中成药的基本原则 (7) 四、儿童使用中成药的基本原则 (7) 第三部分各论 (8) 一、解表剂 (8) 二、泻下剂 (8) 三、和解剂 (8) 四、清热剂 (9) 五、祛暑剂 (9) 六、温里剂 (9) 七、表里双解剂 (10) 八、补益剂 (10) 九、安神剂 (10) 十、开窍剂 (11) 十一、固涩剂 (11) 十二、理气剂 (11) 十三、理血剂 (12) 十四、治风剂 (12) 十五、治燥剂 (12) 十六、祛湿剂 (13) 十七、祛痰剂 (13) 十八、止咳平喘剂 (13) 十九、消导化积剂 (14) 二十、杀虫剂 (14) 第四部分中成药临床应用的管理 (15) 一、含毒性中药材的中成药临床应用的管理 (15) 二、中成药不良反应的监测 (15) 三、开展中成药临床应用监测、建立中成药应用点评制度 (15)

前言 为加强中成药临床应用管理,提高中成药应用水平,保证临床用药安全,国家中医药管理局会同有关部门组织专家制定了《中成药临床应用指导原则》(以下简称《指导原则》)。《指导原则》由四部分组成,第一部分为中成药概述;第二部分为中成药临床应用基本原则;第三部分为各类中成药的特点、适应证及注意事项;第四部分为中成药临床应用的管理。 《指导原则》是为适应中成药临床应用管理需要而制定的,是临床应用中成药的基本原则。每种中成药临床应用的具体要求,还应以药品说明书、最新版本的《中华人民共和国药典》、《中华人民共和国药典-临床用药须知-中药卷》为准。在医疗工作中,临床医师应遵循中医基础理论,根据患者实际情况,选用适宜的药物,辨证辨病施治。 第三部分各论中为更好地说明各类中成药的特点,列举了部分中成药,列举的药物是《国家基本药物目录》中的药物和《国家基本药物目录》未包括但又属临床常用的中成药。 中药注射剂的临床应用及使用管理,《指导原则》提出了具体要求,同时还应遵照《卫生部关于进一步加强中药注射剂生产和临床使用管理的通知》(卫医政发…2008?71号)执行。

养生中药材有哪些

养生中药材有哪些 很多人在养生的时候都会选择用到中药材来帮助自己改善,养生的方法有很多种,但是如果选择中药材来帮助自己养生的话就可以得到很不错的效果,而养生的时候选择中药材也不是什么药材都有养生的效果,这个还得我们细心的挑选,选择专业正规的药材才可以让我们得到养生的好处,那么养生的中药材有哪些呢? 1、人参粥:用人参压成粉末3克、粳米60克、用砂锅煮成粥,可食用。它有益元气,补五脏,生津液、抗衰老的作用。 2、人参茶:用人参10克、大枣10枚,用开水冲泡15分钟后代茶饮用,它有大补元气,安神益智的作用。

3、大枣养生保健应用:大枣津浓厚,其味甘美,营养丰富,药力平和,即是寻常之食品,也是常用之药品,久服或入药膳,确有补气血,益脾胃,通九窍,和百药,润肤养颜,强志延年等养生保健功效。凡体质虚弱或欲邀请书衰延年者均可食用。民间有谚曰:“一日吃三枣,一辈子不显老。”确为经验之谈。它具有护肝、抗肿瘤、中枢抑制、增强肌力等作用。服用大枣的 方法很多, 简单易行的方法有: 1、大枣粥:大枣10枚,茯神15克,小米100克,先 煮大枣及茯神,去渣,后下米煮粥。温食。 2、大枣人参汤:大枣5枚,吉林参(或高丽参)6克。 大枣人参放炖盅内,隔水炖煮1小时。分两次,温热食。人参连用2-3次,救治虚脱,人参加至15-30克,如法炖后,顿服。 在养生的时候这些中药材都是可以的,中药材养生的时

候药材必须要根据医生的要求来给自己配量,让自己吃到最健康的中药材,中药材用来养生的时候也可以选择其他的方法来帮助自己养生,养生的时候也可以多吃一些食物来帮助自己养生,但是最好的方法就是多运动运动,这样才可以得到养生的效果。

煎中药方法大全

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十大泡脚之中药泡脚配方大全 一、泡脚的优点:1、安全;2、无痛苦;3、无毒副作用;4、廉价;5、有效;人们常说“春天洗脚,升阳固脱;夏天洗脚,暑湿可祛;秋天冼脚,肺润肠濡;冬天冼脚,丹田温灼”,哈,这些生活小窍门应该好多人都知道的吧;6、方便;7、舒适。 二、泡脚水的组成:泡脚水—般取自来水、河水、等为基水。通过泡脚治病的可根据不同疾病加入不同的药物。 三、泡脚水的温度,泡脚水的温度以30~38度为宜,但最好不要超过40度。 四、泡脚容器的要求:1、质地应无害、安全、保温性能好。2、高度一般泡脚盆的高度最好超过20厘米[没过踝关节]。3、结构可买一些微电脑浴脚器。 五、泡脚时间的要求:1、每天安排泡脚几次:如一般保健泡脚,每天一次即可;如患有某种疾病每天至少2次以上。2、每天什么时间泡脚为宜:如2次,一般上午lO 点1次,晚上睡前1次,因为睡前泡脚对消除疲劳大有好处可使人睡得更甜容易进入“倒床不复闻钟鼓”的境界。广为流传的“饭后三百步,睡前一盆汤”、“睡前洗脚,胜吃补药”。 3、每次泡脚时间多长为宜:一般为30分钟以上,但对于如慢性风湿性关节炎、慢性高血压等要适当延长一些。每次具体时间还需根据泡脚者的年龄、性别、疾病情况等及泡脚后的感受来逐渐调整。 六、泡脚与按摩的关系:传统的泡脚不包括按摩,现在有了新变化,有些厂家已生产出泡脚与按摩同时进行的泡脚盆,如没买到可用手做一些足底按摩或一些其它按摩这样结合起来效果最好。 七、泡脚的作用:1、清洁皮肤的作用。2、扩血管作用。3、降低血液粘稠度。4、缓解肌肉痉挛。5、镇静作用。 八、泡脚的注意事项:l、注意卫生[最好以家庭为主]。2、切忌求快。3、切忌三天打鱼、两天晒网,要坚持不断才能受益终生。4、儿童禁止泡脚。5、某些急性感染性疾病禁止泡脚。6、出血性疾病禁止泡脚,[包括急性外伤出血,如泡脚会引发意外后果不堪设想]。 高血压:钩藤40克、夏枯草30克、桑叶20克、菊花20克。 失眠:磁石60克、菊花20克、黄芩15克、夜交藤30克。 肝脾肿大:三棱15克、莪术15克、延胡索15克、乌梅10克。 遗精、早泄:仙鹤草40克、黄芩10克、丹皮10克、芡实30克、女贞子30克、狗脊15克、桑葚30克、知母12克、黄柏12克。 足跟、足踝关节痛:寻骨风30克、透骨草30克、鸡血藤30克、乳香10克、没药10克、血竭10克、王不留行15克。 将泡脚方剂煎汤至2000毫升左右,水温保持在40摄氏度上下为宜。

熬中药的最佳方法!在家自己熬中药,放心又省钱

熬中药的最佳方法!在家自己熬中药,放心又省钱 引导语:现在虽然西药已经很普遍的被运用,但是还是很多人对中药深信不疑。尤其对慢性病,很多人还是选择中药治疗。很多大医院都提供了中药代煎服务,殊不知为了提高煎药的效率,很多都只熬一次装袋了事,浪费了药材。在家自己熬中药,放心又省钱。 如何选择熬药的锅 1.熬中药最好的是陶瓷器皿中的砂锅、砂罐,因其化学性质稳定,不易与药物成分发生反应,并且导热均匀,保暖性好。 2.其次可用白色搪瓷器皿或不锈钢锅。 3.煎药忌用铁、铜、铝等金属器具。因为金属元素容易与药液中的中药成分发生化学反应,可能是疗效降低,甚至产生毒副作用。 煎药前的浸泡 药物在煎煮前一定要浸泡使有效成分易于浸出。一般以花、叶、茎类为主的药物,浸泡时间一般为15分钟。以根、种子、根茎、果实类为主的药物浸泡时间一般为半小时。

煎煮次数 以两次或三次为宜。 熬药方法 1.先把药放在砂锅里面,根据药的多少加水,加的水必须漫过中药(千万不要加少了,否则熬中药容易靠干)。大约泡20分钟左右。泡的过程中最好不时用搅拌棒搅一下,这样泡的均匀一些。天热时可以加凉水泡,天冷时用凉水要延长浸泡时间,或者可用温水,这样效果更好邮箱。 2.中药泡好后,放在煤气炉子,或者蜂窝炉子上面开始熬制。在中药熬开之前用大火,熬开之后转为小火慢慢熬,小火熬制大约20分钟。看着表,到时间后,如果药汤还是很多,可以再继续熬一会。切记千万不能把中药熬干了。熬完后,可用一根筷子放在砂锅沿上挡住药渣,再用药淋子过滤,这样效果更好, 3.第二遍熬制时,可以加温水,加的水应是第一次的一半。也是熬20分钟左右,熬完看看药汤多不多,如果不多就可以直接倒出来。若药汤较多,可以再多熬一会儿。 4.有时间的话可以熬第三遍,加的水是第二遍的水的一半。但是一般情况下,熬两遍就可以了,第三遍的药力很低了,但可以熬完用药汤泡脚。 5.在倒中药时,一定要小心烫手。盛中药的器具最好是陶瓷的或不锈钢的,这样中药不易与器具发生化学反应。 煎煮时间

熬中药的方法

1,要选好煎熬中药的容器. 煎熬中药最好是沙锅,陶瓷瓦罐(铝制品,搪瓷器也可用),忌用铁器.因为陶瓷化学性质稳定,在药物水煎复杂的化学应中,不会“干扰”药物的合成与分解,导致影响药效.而我们常用的铁锅容器在药物煎煮过程中,极易同中药内所含的鞣酸质,甙类等成份起反应,造成药物的疗效降低或失效,以至发生反作用,所以不宜使用.一定不要不锈钢或铁锅熬中药.因中药中含有多种生物碱以及各类生物化学物质,尤其在加热条件下,会与不锈钢或铁发生多种化学反应,或使药物失效,甚至产生一定毒性. 2,要掌握正确的煎煮法. 药物入锅后,先用凉水浸泡半小时,使药的有效成份易煎出.放水量要注意,一般放水要高出药面少许,治水肿病的药宜少放水;小孩药要少放水,发汗药可多放水.放水要一次放足,不可中途加凉水,切不可用沸水煮药,以免药物表面蛋白质变性,而影响有效成份析出.煎中草药时,为了使药煎透,最好是加盖煎.尤其是含有挥发性成份的中草药,如薄荷,苏叶,藿香,佩兰等,更要盖好盖,并要在短时间内煎好,以减少有效成份的挥发;有些贵重药物,如人参,鹿茸等也要盖住,并要用文火细煎.煎药要掌握好火候.一般未沸前用急火,沸后用文火.如解表发汗的药,猛火煮沸3~5分即可;熟地,山萸之类补益药则宜用文火煎,煮沸后再煎20分钟左右.此外,绒毛类药物及散剂煎煮时宜做成布包入锅,以减少绒毛对喉的刺激.对于抓的特殊药物,先煎,后煎,冲服,包煎等,都要遵医嘱. 3,要掌握服用方法. 中草药有“冷服”,“热服”之说,服药时间也有讲究.解表药一般宜温服,为了达到发汗的目的;祛寒药也宜热服;解毒药,止咳药,清热药则应冷服;滋补药宜空腹温服,易于消化吸收,但量不宜太多;安神药在睡前半小时,以加强药物作用;脾胃虚弱者宜饭后服药,对胃肠有较强刺激的药物更应饭后服;泻下药须空腹时服,而不宜于夜间服用,大便通畅后则应停药;糖尿病人口渴时服,不拘时间;驱虫药早晚空腹时服,利于驱虫;口腔咽喉病人宜含药,充分发挥药物局部作用;呕吐病宜少量多次饮药,减轻胃的负担,或先服姜汁少许,以降逆止呕;小孩及体弱患者,药量宜少;妇女孕期服药更要谨慎.中药不宜用茶水和乳汁送服,因茶叶,乳汁易和某些药物发生化学作用,降低药效. 4,煎煮中药的要求. ①每次将一剂中药饮片材料放入煲内,加入清水,观察加水能否浸满药面,不足时可稍加水量. ②一般浸泡半小时使中药饮片的有效成分易于煎出(如赶时间,此步骤可略去). ③先用猛火煎至充分沸腾1-3分钟.然后收至小火,煎20-30分钟使之成一碗,用消毒纱布或咖啡格滤渣倒入杯内,温热服用. ④一次将药物煎好后,可以将首剂和再煎的药物混匀,以便药效均衡. 最后一定注意服用的时间,应当仔细询问医生,记在纸上.

十大泡脚之中药泡脚配方大全

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因为睡前泡脚对消除疲劳大有好处可使人睡得更甜容易进入“倒床不复闻钟鼓”的境界。广为流传的“饭后三百步,睡前一盆汤”、“睡前洗脚,胜吃补药”。3、每次泡脚时间多长为宜:一般为30分钟以上,但对于如慢性风湿性关节炎、慢性高血压等要适当延长一些。每次具体时间还需根据泡脚者的年龄、性别、疾病情况等及泡脚后的感受来逐渐调整。 六、泡脚与按摩的关系:传统的泡脚不包括按摩,现在有了新变化,有些厂家已生产出泡脚与按摩同时进行的泡脚盆,如没买到可用手做一些足底按摩或一些其它按摩这样结合起来效果最好。 七、泡脚的作用:1、清洁皮肤的作用。2、扩张血管作用。 3、降低血液粘稠度。 4、缓解肌肉痉挛。 5、镇静作用。 八、泡脚的注意事项:l、注意卫生[最好以家庭为主]。2、切忌求快。3、切忌三天打鱼、两天晒网,要坚持不断才能受益终生。 4、儿童禁止泡脚。 5、某些急性感染性疾病禁止泡脚。 6、出血性疾病禁止泡脚,[包括急性外伤出血,如泡脚会引发意外后果不堪设想]。 高血压:钩藤40克、夏枯草30克、桑叶20克、菊花20克。

标准的水煎中药法

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