194 research outputs found
Influence of irrigated agriculture on soil carbon and microbial community structure
Increasing the amount of carbon (C) in soils is
one method to reduce the concentration of carbon dioxide
(CO2) in the atmosphere. We measured organic C stored in
southern Idaho soils having long-term cropping histories that
supported native sagebrush vegetation (NSB), irrigated moldboard
plowed crops (IMP), irrigated conservation-chisel-tilled
crops (ICT), and irrigated pasture systems (IP). The CO 2 emitted
as a result of fertilizer production, farm operations, and
CO2 lost via dissolved carbonate in irrigation water, over a
30-year period, was estimated and used to calculate net C
fixation. Organic C in ecosystems decreased in the order
IP>ICT>IMP> NSB. In February 2001, active fungal, bacterial,
and microbial biomass was greater in IP soils than all
other soils. Active fungal, bacterial, and microbial biomass
was least in ICT soils at the 15-30-cm depth than all other
soils. In August 2001, active bacterial biomass was greater in
IMP soils than IP, ICT, and NSB soils. Active fungal biomass
was greater in IP soils than all other soils. Whole-soil fatty acid
profiles differed among management regimes and sampling
dates and, to a lesser extent, with soil depth. FAME profiles
from the NSB soils were distinct from the agricultural treatments
and contained greater amounts of total fatty acids than
the other treatments. The IMP and ICT soils yielded fatty acid
profiles that were similar to each other, although those at the
15-30-cm depth were distinct from all other treatment-depth
combinations. The IP FAME profiles suggest that arbuscular
mycorrhizal fungi are more common in these soils than soils
from the other treatments. Differences in carbon substrate
utilization patterns (BIOLOG) among treatments were more
variable and less pronounced that FAME results. In general,
irrigated arid soils can both increase C storage while increasing
microbial biomass and changing microbial diversity
The influence of vegetation in riparian filterstrips on coliform bacteria: II. Survival in soils
Survival of total and fecal coliform bacteria was measured in the
0 to 5, 5 to 15, and 15 to 30 cm soil depths at 1, 3, 7, 14, and 90 to
120 d after swine (Sus scrofa) wastewater application to riparian
filterstrips in southern Georgia during each season of the year. Vegetative
treatments evaluated were: (i) 20 m grass-10 m forest, (ii) 10 m
grass-20 m forest, and (iii) 10 m grass-20 m maidencane (Panicum
hemitomon Schult.). During winter, spring, and summer vegetation
type in riparian filterstrips did not affect survival of total and fecal
coliform bacteria. Total and fecal coliform bacterial numbers were
usually higher in the top 0 to 5 cm of soil than in the 5 to 15 and 15
to 30 cm soil depths in all treatments. Total and fecal coliform numbers
in the 0 to 5, 5 to 15, and 15 to 30 cm depths declined approximately
10-fold every 7 to 14 d after waste application in all seasons of the
year. At 90 to 120 d after waste application, total and fecal coliform
numbers in the three soil depths did not differ from riparian filterstrips
that did not have animal waste applied. Total coliform bacteria in the
O to 5, 5 to 15, and 15 to 30 cm soil depths correlated with temperature
and moisture in a curvilinear relationship (r2 = 0.80 , 0.77, and 0.64,
respectively). Fecal coliform bacteria in 0 to 5, 6 to 15, and 16 to 30 cm
of soil also correlated with temperature and moisture in a curvilinear
relationship (r 2 = 0.56 , 0.53, and 0.53, respectively)
The influence of vegetation in riparian filterstrips on coliform bacteria: I. Movement and survival in water
Swine (Sus scrofa) wastewater was applied to three separate 4 m
wide x 30 m long riparian filterstrips consisting of 20 m grass and
10 m forest, 10 m grass and 20 m forest, and 10 m grass and 20 m
maidencane (Panicum hemitomon Schult.) in Southern Georgia during
each season. Total and fecal coliform numbers in the applied
wastewater pulse did not decline as water moved downslope regardless
of vegetation type or season. The pulse of applied wastewater did
not move beyond 15 m in any treatment in autumn or summer (dry
seasons) and only moved beyond 7.5 m in the 20 m grass-10 m forest
treatment in the summer. Total and fecal coliform numbers in soil
water and shallow ground water declined by approximately 10-fold
every 7 d for the first 14 d regardless of vegetative treatment or season.
Soil temperature and soil moisture correlated with total coliform
bacteria in both 13 m wells (r2 = 0.89) and 2.0 m wells (r2 = 0.89),
and with fecal coliform bacteria in 1.5 (r2 = 0.82) and 2.0 m (r2 =
0.76) wells. Animal production operations may need to locate in
warm–dry climates so animal waste can be applied to lands to help
ensure enteric bacteria input to surface and ground water will not
occur
Influence of C02 enrichment and nitrogen fertilization on tissue chemistry and carbon allocation in longleaf pine seedlings
One-year old, nursery-grown longleaf pine (Pinus palustris Mill.) seedlings were grown in 45-L pots containing a
coarse sandy medium and were exposed to two concentrations of atmospheric CO2 (365 or 720 µmol?1) and two
levels of nitrogen (N) fertility (40 or 400 kg N ha?1 yr?1) within open top chambers for 20 months. At harvest,
needles, stems, coarse roots, and fine roots were separated and weighed. Subsamples of each tissue were frozen
in liquid N, lyophilized at ?50 ?C, and ground to pass a 0.2 mm sieve. Tissue samples were analyzed for carbon
(C), N, nonpolar extractives (fats, waxes, and oils = FWO), nonstructural carbohydrates (total sugars and starch),
and structural carbohydrates (cellulose, lignin, and tannins). Increased dry weights of each tissue were observed
under elevated CO2 and with high N; however, main effects of CO2 were significant only on belowground tissues.
The high N fertility tended to result in increased partitioning of biomass aboveground, resulting in significantly
lower root to shoot ratios. Elevated CO2 did not affect biomass allocation among tissues. Both atmospheric CO2
and N fertility tended to affect concentration of C compounds in belowground, more than aboveground, tissues.
Elevated CO2 resulted in lower concentrations of starch, cellulose, and lignin, but increased concentrations of
FWO in root tissues. High N fertility increased the concentration of starch, cellulose, and tannins, but resulted in
lower concentrations of lignin and FWO in roots. Differences between CO2 concentrations tended to occur only
with high N fertility. Atmospheric CO2 did not affect allocation patterns for any compound; however the high N
treatment tended to result in a lower percentage of sugars, cellulose, and lignin belowgroun
Polyacrylamide (PAM) - A one million acre progress report
Water soluble polyacrylamide (PAM) was recognized in the early 1990s as an environmentally safe
and highly effective erosion-preventing and infiltration-enhancing chemical, when applied in very
dilute concentrations in furrow irrigation water (Lentz et al., 1992; Lentz and Sojka, 1994;
McCutchan et al., 1994; Trout et al., 1995; Sojka and Lentz, 1997; Sojka et al., 1998a,b). The mode
of action involves surface soil structure stabilization and maintenance of pore continuity. A
recommended conservation practice standard was published by NRCS in 1995 (Anonymous, 1995)
and is being revised in 1999. It delineates considerations and specifies methodology for. PAM-use.
Commercial sales of erosion-preventing PAMs began in 1995. Approximately one million acres
were treated in the United States in 1999. Extent of adoption of the practice outside the US is less
certain, but interest is growing in several countries and continents. Key aspects of this PAM
technology development are presented below
An ecoinformatics tool for microbial community studies: Supervised classification of amplicon length heterogeneity (ALH) profiles of 16S rRNA
Support vector machines (SVM) and K-nearest neighbors (KNN) are two computational machine learning tools that
perform supervised classification. This paper presents a novel application of such supervised analytical tools for microbial
community profiling and to distinguish patterning among ecosystems. Amplicon length heterogeneity (ALH) profiles from
several hypervariable regions of 16S rRNA gene of eubacterial communities from Idaho agricultural soil samples and from
Chesapeake Bay marsh sediments were separately analyzed. The profiles from all available hypervariable regions were
concatenated to obtain a combined profile, which was then provided to the SVM and KNN classifiers. Each profile was
labeled with information about the location or time of its sampling. We hypothesized that after a learning phase using
feature vectors from labeled ALH profiles, both these classifiers would have the capacity to predict the labels of previously
unseen samples. The resulting classifiers were able to predict the labels of the Idaho soil samples with high accuracy. The
classifiers were less accurate for the classification of the Chesapeake Bay sediments suggesting greater similarity within the
Bay's microbial community patterns in the sampled sites. The profiles obtained from the VI +V2 region were more
informative than that obtained from any other single region. However, combining them with profiles from the V1 region
(with or without the profiles from the V3 region) resulted in the most accurate classification of the samples. The addition
of profiles from the V9 region appeared to confound the classifiers. Our results show that SVM and KNN classifiers can
be effectively applied to distinguish between eubacterial community patterns from different ecosystems based only on their
ALH profiles
Experimental system to displace radioisotopes from upper to deeper soil layers: chemical research
BACKGROUND: Radioisotopes are introduced into the environment following nuclear power plant accidents or nuclear weapons tests. The immobility of these radioactive elements in uppermost soil layers represents a problem for human health, since they can easily be incorporated in the food chain. Preventing their assimilation by plants may be a first step towards the total recovery of contaminated areas. METHODS: The possibility of displacing radionuclides from the most superficial soil layers and their subsequent stabilisation at lower levels were investigated in laboratory trials. An experimental system reproducing the environmental conditions of contaminated areas was designed in plastic columns. A radiopolluted soil sample was treated with solutions containing ions normally used in fertilisation (NO(3)(-), NH(4)(+), PO(4)(--- )and K(+)). RESULTS: Contaminated soils treated with an acid solution of ions NO(3)(-), PO(4)(--- )and K(+), undergo a reduction of radioactivity up to 35%, after a series of washes which simulate one year's rainfall. The capacity of the deepest soil layers to immobilize the radionuclides percolated from the superficial layers was also confirmed. CONCLUSION: The migration of radionuclides towards deeper soil layers, following chemical treatments, and their subsequent stabilization reduces bioavailability in the uppermost soil horizon, preventing at the same time their transfer into the water-bearing stratum
Litterfall, litter decomposition and associated nutrient fluxes in Pinus halepensis: influence of tree removal intensity in a Mediterranean forest
The online version of this
article (doi:10.1007/s10342-015-0893-z) contains supplementary
material, which is available to authorized users[EN] Our knowledge about the influence of silvicultural treatments on nutrient cycling processes in Mediterranean forests is still limited. Four levels of tree removal were compared in an Aleppo pine forest in eastern Spain to determine the effects on litterfall, litter decomposition and the associated nutrient fluxes after 12 years. Removal treatments included clearfelling, two shelterwood intensities (60 and 75 % of basal area removed) and untreated controls. Twelve years later, the basal area removed still explained 60 % of litterfall mass variance and 60 % of C, 52 % of N, 45 % of P, 17 % of K, 47 % of Ca and 60 % of Mg return variances. Litter decomposed somewhat more slowly in clearfellings compared to controls (p = 0.049), accumulated more Ca and released less K compared to the other three treatments. This was explained by contamination with mineral particles due to the poorly developed O horizon in clearfellings. We conclude that the management practices reduced the nutrient return via litterfall, but the nutrient release through decomposition seems poorly sensitive to canopy disturbance. In order to accurately quantify the harvesting impacts on nutrient cycling in this Mediterranean forest system, it is necessary to measure the litterfall of the understory layer.This work has been supported by a fellowship from the Generalitat Valenciana, Conselleria de Educacion, Formacion y Empleo awarded to L. Lado-Monserrat (BFPI/2008/041). Silvicultural treatments were carried out by the Mediterranean Centre for Environmental Studies (CEAM) through programme "I + D en relacion con la restauracion de la cubierta vegetal y otros aspectos de investigacion forestal". Dataloggers and probes were provided by the Generalitat Valenciana through Project "Efecto de diferentes sistemas de aclareo de masa forestal sobre la disponibilidad de agua, nutrientes y la regeneracion de la masa arborea y arbustiva en parcelas de pinar" (GV06/126). We acknowledge Joana Oliver, Ruth M. Tavera and Daniel Fortanet for their help in the laboratory and in the field. The authors wish to thank Francisco Galiana for his assistance, including help in fieldwork and providing information about the experimental design of the silvicultural treatments. Thanks also go to Rafael Herrera from the Centro de Ecologia, Instituto Venezolano de Investigaciones Cientificas, Caracas, Venezuela and two anonymous reviewers for critically reviewing the manuscript.Lado Monserrat, L.; LidĂłn, A.; Bautista, I. (2015). Litterfall, litter decomposition and associated nutrient fluxes in Pinus halepensis: influence of tree removal intensity in a Mediterranean forest. European Journal of Forest Research. 134(5):833-844. https://doi.org/10.1007/s10342-015-0893-zS8338441345Almagro M, MartĂnez-Mena M (2012) Exploring short-term leaf-litter decomposition dynamics in a Mediterranean ecosystem: dependence on litter type and site conditions. Plant Soil 358:323–335Alvarez A, Gracia M, Vayreda J, Retana J (2012) Patterns of fuel types and crown fire potential in Pinus halepensis forests in the Western Mediterranean Basin. For Ecol Manage 270:282–290Austin AT, Vivanco L (2006) Plant litter decomposition in a semi-arid ecosystem controlled by photodegradation. Nature 442:555–558Bates JD, Svejcar TS, Miller RF (2007) Litter decomposition in cut and uncut western juniper woodlands. J Arid Environ 70:222–236Binkley D (2008) Three key points in the design of forest experiments. For Ecol Manage 255:2022–2023Blair JM, Crossley DA Jr (1988) Litter decomposition, nitrogen dynamics and litter microarthropods in a southern Appalachian hardwood forest 8 years following clearcutting. J Appl Ecol 25:683–698Blanco JA, Zavala MA, Imbert JB, Castillo FJ (2005) Sustainability of forest management practices: evaluation through a simulation model of nutrient cycling. For Ecol Manage 213:209–228Blanco JA, Imbert JB, Castillo FJ (2006) Influence of site characteristics and thinning intensity on litterfall production in two Pinus sylvestris L. forests in the western Pyrenees. For Ecol Manage 237:342–352Blanco JA, Imbert JB, Castillo FJ (2008) Nutrient return via litterfall in two contrasting Pinus sylvestris forests in the Pyrenees under different thinning intensities. For Ecol Manage 256:1840–1852Blanco JA, Imbert JB, Castillo FJ (2011) Thinning affects Pinus sylvestris needle decomposition rates and chemistry differently depending on site conditions. Biogeochemistry 106:397–414Caldentey J, Ibarra M, Hernández J (2001) Litter fluxes and decomposition in Nothofagus pumilio stands in the region of Magallanes, Chile. For Ecol Manage 148:145–157Christensen JH, Krishna Kumar K, et al. (2013) Climate phenomena and their relevance for future regional climate change. In: Stocker TF, Qin D, Plattner G-K et al (Eds.) Climate change 2013: the physical science basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USACortina J, Vallejo VR (1994) Effects of clearfelling on forest floor accumulation and litter decomposition in a radiata pine plantation. For Ecol Manage 70:299–310Entry JA, Rose CL, Cromack K Jr (1991) Litter decomposition and nutrient release in ectomycorrhizal mat soils of a Douglas fir ecosystem. Soil Biol Biochem 23:285–290Fabbio G, Merlo M, Tosi V (2003) Silvicultural management in maintaining biodiversity and resistance of forests in Europe—the Mediterranean region. J Environ Manage 67:67–76Galiana F, PĂ©rez-BadĂa R, Camarero E, Estruch V, Currás R (2001) EstimaciĂłn de la RadiaciĂłn solar incidente en pinares de Pinus halepensis sometidos a tratamientos selvĂcolas de cortas finales. In: Junta de AndalucĂa. ConsejerĂa de Medio Ambiente (Ed.) Actas del III Congreso Forestal Español. Junta de AndalucĂa. Granada (Original in Spanish)GarcĂa-PlĂ© C, Vanrell P, Morey M (1995) Litter fall and decomposition in a Pinus halepensis forest on Mallorca. J Veg Sci 6:17–22González Utrillas N, González PĂ©rez E, Galiana F (2005) VariaciĂłn del crecimiento diametral de la masa de pinar de carrasco en cortas finales experimentales, en los montes de Tuejar y Chelva (Valencia). IV Congreso Forestal Español. Zaragoza. Soc. Esp. Cien. For. (Original in Spanish)Guo LB, Sims REH (1999) Litter decomposition and nutrient release via litter decomposition in New Zealand eucalypt short rotation forests. Agric Ecosyst Environ 75:133–140GVA (1995) Mapa de Suelos de la Comunidad Valenciana. Chelva (666). Proyecto LUCDEME (Icona), Centro de Investigaciones sobre DesertificaciĂłn y Conselleria d’Agricultura i Mig Ambient. Generalitat Valenciana. Valencia, Spain. (Original in Spanish)Hennessey TC, Dougherty PM, Cregg BM, Wittwer RF (1992) Annual variation in needle fall of a loblolly pine stand in relation to climate and stand density. For Ecol Manage 51:329–338Inagaki Y, Kuramoto S, Torii A, Shinomiya Y, Fukata H (2008) Effects of thinning on leaf-fall and leaf-litter nitrogen concentration in hinoki cypress (Chamaecyparis obtusa Endlicher) plantation stands in Japan. For Ecol Manage 255:1859–1867Jonard M, Misson L, Ponette Q (2006) Long-term thinning effects on the forest floor and the foliar nutrient status of Norway spruce stands in the Belgian Ardennes. Can J For Res 36:2684–2695Kim C, Sharik TL, Jurgensen MF (1996a) Canopy cover effects on mass loss, and nitrogen and phosphorus dynamics from decomposing litter in oak and pine stands in northern Lower Michigan. For Ecol Manage 80:13–20Kim C, Sharik TL, Jurgensen MF (1996b) Litterfall, nitrogen and phosphorus inputs at various levels of canopy removal in oak and pine stands in northern lower Michigan. Am Midl Nat 135:195–204Kim C, Son Y, Lee WK, Jeong J, Noh NJ, Kim SR, Yang AR, Ju NG (2012) Influence of forest tending (Soopkakkugi) works on litterfall and nutrient inputs in a Pinus densiflora stand. For Sci Technol 8:83–88Kimmins JP (2004) Forest ecology, a foundation for sustainable management and environmental ethics in forestry. Prentice-Hall, New JerseyKimmins JP, Mailly D, Seely B (1999) Modelling forest ecosystem net primary production: the hybrid simulation approach used in FORECAST. Ecol Modell 122:195–224Klemmedson JO, Meier CE, Campbell RE (1990) Litter fall transfers of dry matter and nutrients in ponderosa pine stands. Can J For Res 20:1105–1115Kunhamu TK, Kumar BM, Viswanath S (2009) Does thinning affect litterfall, litter decomposition, and associated nutrient release in Acacia mangium stands of Kerala in peninsular India? Can J For Res 39:792–801Lytle DE, Cronan CS (1998) Comparative soil CO2 evolution, litter decay, and root dynamics in clearcut and uncut spruce–fir forest. For Ecol Manage 103:121–128Molina AJ, Del Campo AD (2012) The effects of experimental thinning on throughfall and stemflow: a contribution towards hydrology-oriented silviculture in Aleppo pine plantations. For Ecol Manage 269:206–213Navarro FB, Romero-Freire A, Del Castillo T, Foronda A, JimĂ©nez MN, Ripoll MA, Sánchez-Miranda A, Hutsinger L, Fernández-Ondoño E (2013) Effects of thinning on litterfall were found after years in a Pinus halepensis afforestation area at tree and stand levels. For Ecol Manage 289:354–362Olson JS (1963) Energy storage and the balance of producers and decomposers in ecological systems. Ecology 44:322–331PĂ©rez Cueva AJ (1994) Atlas Climático de la Comunidad Valenciana. ColecciĂłn Territori nÂş 4. Generalitat Valenciana. Conselleria d’Obres Publiques, Urbanisme i Transport, ValenciaPetritsch R, Hasenauer H, Pietsch SA (2007) Incorporating forest growth response to thinning within biome-BGC. For Ecol Manage 242:324–336Prescott CE (1997) Effects of clearcutting and alternative silvicultural systems on rates of decomposition and nitrogen mineralization in a coastal montane coniferous forest. For Ecol Manage 95:253–260Prescott CE (2002) The influence of the forest canopy on nutrient cycling. Tree Physiol 22:1193–1200Prescott CE, Blevins LL, Staley CL (2000) Effects of clear-cutting on decomposition rates of litter and forest floor in forests of British Columbia. Can J For Res 30:1751–1757Roig S, Del RĂo M, Cañellas I, Montero G (2005) Litter fall in Mediterranean Pinus pinaster Ait. stands under different thinning regimes. For Ecol Manage 206:179–190Sardans J, Peñuelas J, RodĂ F (2005) Changes in nutrient use efficiency, status and retranslocation in young post-fire regeneration Pinus halepensis in response to sudden N and P input, irrigation and removal of competing vegetation. Trees 19:233–250Scarascia-Mugnozza G, Oswald H, Piussi P, Radoglou K (2000) Forests of the Mediterranean region: gaps in knowledge and research needs. For Ecol Manage 132:97–109Slovik S (1997) Tree physiology. In: HĂĽttl RF, Schaaf W (eds) Magnesium deficiency in forest ecosystems. Kluwer Academic Publishers, London, pp 101–214Taylor BR, Parkinson D (1988) Does repeated freezing and thawing accelerate decay of leaf litter? Soil Biol Biochem 20:657–665Torras O, Saura S (2008) Effects of silvicultural treatments on forest biodiversity indicators in the Mediterranean. For Ecol Manage 255:3322–3330Trofymow JA, Barclay HJ, McCullough KM (1991) Annual rates and elemental concentrations of litter fall in thinned and fertilized Douglas-fir. Can J For Res 21:1601–1615Wallace ES, Freedman B (1986) Forest floor dynamics in a chronosequence of hardwood stands in central Nova Scotia. Can J For Res 16:293–302Whitford WG, Meentemeyer V, Seastedt TR, Cromack Jr K, Crossley Jr DA, Santos P, Todd RL, Waide JB (1981) Exceptions to the AET model: deserts and clear-cut forest. Ecology 62:275–277Yin X, Perry JA, Dixon RK (1989) Influence of canopy removal on oak forest floor decomposition. Can J For Res 19:204–21
Effect of Biocontrol Agent Pseudomonas fluorescens 2P24 on Soil Fungal Community in Cucumber Rhizosphere Using T-RFLP and DGGE
Fungi and fungal community play important roles in the soil ecosystem, and the diversity of fungal community could act as natural antagonists of various plant pathogens. Biological control is a promising method to protect plants as chemical pesticides may cause environment pollution. Pseudomonas fluorescens 2P24 had strong inhibitory on Rastonia solanacearum, Fusarium oxysporum and Rhizoctonia solani, etc., and was isolated from the wheat rhizosphere take-all decline soils in Shandong province, China. However, its potential effect on soil fungal community was still unknown. In this study, the gfp-labeled P. fluorescens 2P24 was inoculated into cucumber rhizosphere, and the survival of 2P24 was monitored weekly. The amount decreased from 108 to 105 CFU/g dry soils. The effect of 2P24 on soil fungal community in cucumber rhizosphere was investigated using T-RFLP and DGGE. In T-RFLP analysis, principle component analysis showed that the soil fungal community was greatly influenced at first, digested with restriction enzyme Hinf I and Taq I. However, there was little difference as digested by different enzymes. DGGE results demonstrated that the soil fungal community was greatly shocked at the beginning, but it recovered slowly with the decline of P. fluorescens 2P24. Four weeks later, there was little difference between the treatment and control. Generally speaking, the effect of P. fluorescens 2P24 on soil fungal community in cucumber rhizosphere was just transient
- …