ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 11
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 85 (1981), S. 201-207 
    ISSN: 1573-5117
    Keywords: floating plants ; submersed plants ; emersed plants ; aquatic systems ; physico-chemical parameters ; euthropic lake
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract A field study was conducted during the months of October, January, May, and July (1979–80) to examine the diel variations in dissolved O2 (DO), pH, dissolved CO2, bicarbonate and carbonate alkalinity, NH4-N, NO3-N, and PO4-P concentration, and conductivity (EC) of the water in six aquatic systems. Water in hyacinth (Eichhornia crassipes) ponds showed very little or no diel or seasonal variations in DO, pH, dissolved CO2, and bicarbonate alkalinity. Dissolved O2 concentration of the water under floating hyacinth cover was in the range of 0.2–3.0 µg/ml, while dissolved CO2 levels were in the range of 10–35 µg/ml. In the aquatic systems with no floating vegetation, i.e., elodea (Egeria densa) pond, cattail (Typha sp.) pond, control pond (filamentous algae and Chara spp.), and eutrophic lake (algae in Lake Apopka), DO and pH of the water increased during mid-day and decreased during the night. Dissolved O2 levels in these ponds were in the range of 5–20 µg/ml during mid-day and 2–8 µg/ml during the night, while pH of the water was in the range of 8–9.5 during mid-day and decreased to 7–8 during the night. An inverse relationship was observed between bicarbonate and carbonate alkalinity of the water in the aquatic systems with no floating vegetation while no carbonates were detected in the water with floating hyacinth plants. Ammonium N, NO3-N and PO4-P concentration of the water in these aquatic systems showed very little or no diel variations.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 12
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 98 (1983), S. 237-243 
    ISSN: 1573-5117
    Keywords: detention pond ; treatment system ; drainage water ; flooded soils ; organic soil
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Nitrogen and P interchange between the sediments and the overlying water of a simulated retention pond used for wastewater treatment were evaluated under conditions of seasonal temperature fluctuations and varying physico-chemical conditions (exposing floodwater surface to daylight vs. dark and turbulent vs. quiscent floodwater). Natural sediment columns obtained from two types of field retention ponds were used. One type of retention pond consisted of calcareous clay loam sediment while the sediment of second retention pond contained organic soil. Nutrient interchange between sediments and the overlying water was measured once a month over a period of one year. Nitrogen removal rates from floodwater were controlled by the initial floodwater NH 4 + and NO 3 − concentration, rate of NH 4 + diffusion from the sediments to the overlying water, ammonification in the sediments, NH3 volatilization and nitrification at the sediment-water interface, and denitrification in the sediments. Under the conditions studied, NH 4 + concentrations of the floodwater were in the range of 0.01 to 0.05 µg/ml, while NO 3 − concentrations were in the range of 0.27 to 0.78 µg/ml. Sediments with organic soil were found to be less effective in the removal of floodwater organic N, organic C and P, compared to the sediments with calcareous clay loam. Phosphorus exchange rates were dependent on the capacity of the sediment to adsorb or desorb P. Total P exchange rates were in the range of −1.04 to 0.34 mg P/m2 day. Seasonal temperature fluctuations, turbulent vs. quiscent water conditions or exposing the floodwater surface to daylight or dark had very little effect on N and P exchange rates.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 13
    Electronic Resource
    Electronic Resource
    Springer
    Plant growth regulation 20 (1996), S. 179-183 
    ISSN: 1573-5087
    Keywords: cotton ; growth ; mepiquat chloride ; photosynthesis ; PIX ; RuBP carboxylase
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Mepiquat chloride (N, N-dimethylpiperidinium chloride), well known as PIX, is a potential systemic plant growth regulator. The effects of PIX on plant height, stem elongation, leaf area, net photosynthetic rates, chlorophyll content, sucrose and starch levels, and RuBP carboxylase activity in cotton (Gossypium hirsutum L. cv. DES 119) plants were measured. PIX was sprayed (0, 7.65, 15.3, 30.6 or 61.2 g active ingredient ha−1) on the plants at first square (25 days after emergence) and measurements were made at frequent intervals. Plant height was clearly reduced by PIX. The total length of vegetative branches and fruiting branches was 40% and 50% less than the control. Total leaf area in PIX treated plants was 16% less than the control. Net photosynthetic rates were 25% less in PIX-treated leaves. PIX treated leaves had more chlorophyll content. The activity of RuBP carboxylase was decreased in PIX treated plants. Starch accumulation was noticed in PIX treated leaves while sucrose content was not changed. The data reported here suggest that reduced growth responses induced by PIX results in partial loss of photosynthetic capacity in cotton at least up to 20 days after application of the growth regulator.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 14
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 129 (1990), S. 269-276 
    ISSN: 1573-5036
    Keywords: CH4 emissions ; denitrification ; gas entrapment ; rice soils ; stable N isotopes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract In a field experiment using microplots, a flooded Crowley silt loam (Typic Albaqualfs) rice soil was fertilized with 15N labelled (60–74 atom %) urea and KNO3. Emission of N2, N2O and CH4 and accumulation in soil were measured for 21 d after fertilizer application. Emission of 15N2-N measured from the urea and KNO3 treated plots ranged from 〈15 to 570 and from 330 to 3,420 g ha−1 d−1, respectively. Entrapped 15N2-N in the urea treated microplots was significantly lower (〈15 g to 2.1 kg ha−1) on all sampling dates compared to the 15N2-N gas accumulation in the KNO3 treated plots (6.4 to 31.5 kg ha−1). Emissions of N2O-N were low and did not exceed 4 g ha−1 d−1. Fluxes of CH4 from the fertilizer and control plots were low and never exceeded 33 g ha−1 d−1. Maximum accumulation of CH4 in the flooded soil measured 460 and 195 g ha−1 for the urea and KNO3 treatments, respectively.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 15
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 49 (1978), S. 409-415 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Short-term experiments were conducted to determine the effect of varying levels of iron and manganese on65Zn absorption by roots and translocation to shoots in soybean seedlings. In 11 hours uptake duration, both iron and manganese depressed the65Zn absorption by roots and translocation to shoots. The depression was of higher magnitude at higher levels of iron and manganese (5.0 ppm) in the medium coupled with highest level (5.0 ppm) of zinc concentration. It is concluded that interactions between zinc and iron as well as zinc and manganese occur during absorption and translocation processes.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 16
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 57 (1980), S. 375-381 
    ISSN: 1573-5036
    Keywords: Ammonium ; Fertilizer-N efficiency ; Flooded soils ; Native soil N ; N-15 isotope ; N loss ; Uptake ; Urea
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract Data from five field experiments using labelled nitrogen fertilizer were used to determine the relative effects of soil nitrogen and fertilizer nitrogen on rice yield. Yield of grain was closely correlated with total aboveground nitrogen uptake (soil+fertilizer), less closely correlated with soil nitrogen uptake and not significantly correlated with fertilizer nitrogen uptake. When yield increase rather than yield was correlated with fertilizer nitrogen uptake, the correlation coefficient was statistically significant.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 17
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 67 (1982), S. 209-220 
    ISSN: 1573-5036
    Keywords: Ammonification ; Crop residues ; Denitrification ; Flooded soil ; 15-N ; N-fertilizers ; N2-fixation ; Nitrification ; Rice ; Volatilization
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Description / Table of Contents: Resumen Se revisaron varios aspectos del ciclo de nitrógeno estudiados con15N en un ecosistema de arroz de innundación en suelos franco limosos Crowley en Louisiana, USA, conel fin de construir un balance de masas para el nitrógeno. Las tranformaciones que se incluyeron en el modelo fueron: 1) amonificación neta (0,22 mg NH4−N kg−1 suelo seco dia−1), 2) nitrificación neta (2,07 mg NO3−N kg−1 suelo seco dia−1), 3) desnitrificación (0,37 mg N kg−1 suelo seco dia−1) y 4) fijación biológica de nitrógeno (0,16 mg N kg−1 suelo seco dia−1). Las entradas de nitrógeno al sistema serían aquellas por aplicación de fertilizantes, incorporación de residuos de cosecha, fijación biológica de nitrógeno, deposición. Las salidas serían por cosecha, perdidas gaseosas por volatilización de NH3 y la ocurrencia simultanea de nitrificación y desnitrificación, lixiviación y escorrentía. El balance de masas indicó que el 33% del nitrógeno inorgánico disponible fué recuperado por el arroz y el resto se perdió del sistema. Las pérdidas por volatilización de NH3 fueron minimas porque el fertilizante fué incorporado al suelo. Una proporción significativa del nitrógeno inorgánico se perdió por difusión de NH4 de la capa anaeróbica a la aeróbica en respuesta al gradiente de concentraciones; luego ocurre nitrificación en la capa aeróbica, difusión y finalmente desnitrificación y pérdida en forma gaseosa. Las perdidas por lixiviación y escorrentía fueron minimas.
    Notes: Abstract 15N studies of various aspects of the nitrogen cycle in a flooded rice ecosystem on Crowley silt loam soil in Louisiana were reviewed to construct a mass balance model of the nitrogen cycle for this system. Nitrogen transformations modeled included 1) net ammonification (0.22 mg NH4 +−N kg dry soil−1 day−1), 2) net nitrification (2.07 mg NO3 −−N kg−1 dry soil−1 day−1), 3) denitrification (0.37 mg N kg dry soil−1 day−1), and 4) biological N2 fixation (0.16 mg N kg dry soil−1 day−1). Nitrogen inputs included 1) application of fertilizers, 2) incorporation of crop residues, 3) biological N2 fixation, and 4) deposition. Nitrogen outputs included 1) crop removal, 2) gaseous losses from NH3 volatilization and simultaneous occurrence of nitrification-denitrification, and 3) leaching and runoff. Mass balance calculations indicated that 33% of the available inorganic nitrogen was recovered by rice, and the remaining nitrogen was lost from the system. Losses of N due to ammonia volatilization were minimal because fertilizer-N was incorporated into the soil. A significant portion of inorganic-N was lost by ammonium diffusion from the anaerobic layer to the aerobic layer in response to a concentration gradient and subsequent nitrification in the aerobic layer followed by nitrate diffusion into the anaerobic layer and denitrification into gaseous end products. Leaching and surface runoff losses were minimal.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 18
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 19
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 211 (1991), S. 101-109 
    ISSN: 1573-5117
    Keywords: aquatic plants ; Eichhornia crassipes ; eutrophic lake water ; biomass ; carbon mineralization ; nitrogen mineralization
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract A study was conducted to determine the seasonal production of detritus by water hyacinths [Eichhornia crassipes (Mart.) Sohns] cultured in eutrophic Lake Apopka water, and the decomposition of detritus in situ and under laboratory conditions. Annual averages for C, N and P deposited through detritus production at the sediment-water interface were 2870, 176 and 19 kg ha-1 yr-1, respectively. Decomposition rates were faster in the root zone of hyacinth mats than at the sediment-water interface. Approximately 92% of the detritus C deposited at the sediment-water interface was decomposed in one year, while only 11% of the detrital organic N was mineralized. Detrital tissue gained P during decomposition, suggesting P limitation for the system. Dry-weight loss of detrital tissue was significantly correlated with the mass of C lost (r 2 = 0.947**), C/N ratio (r 2 = 0.644**) and C/P ratio (r 2 = 0.428**).
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 20
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 345 (1997), S. 45-57 
    ISSN: 1573-5117
    Keywords: P sorphon kinetics ; redox potential (Eh) ; lake sediments ; P fractions ; mineral P equilibria ; eutrophic lakes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Biogeochemical reactions in shallow eutrophic lakes areaffected bythe changes in redox potential (Eh) as bottom sedimentsundergotemporal resuspension and settling. The stability of varioussediment P fractions and kinetics of P-uptake were evaluatedfortwo sub-tropical lakes (Lake Apopka and Lake Okeechobee,Florida)using sediment suspensions in closed systems maintained atvariousEh levels ranging from −235 to 555 mV. Redox potential hadminimal effect on the stability of NaOH-P (Fe-/Al-bound P plusmoderately resistant organic P) and HCl-P (Ca-/Mg-P) fractionsinLake Apopka sediments. Increases in ortho-P and NH4Cl-P(loosely-bound P plus labile organic P) concentrations wereobserved in highly reduced (Eh = −225 mV) Apopkasediments.Phosphate solubility diagrams and mineral equilibriacalculationssuggest that P-uptake by Apopka bottom sediments at elevated Pconcentrations (ortho-P ≤ 110 μM) was due toformationof Ca-P compounds and/or co-precipitation of P withCaCO3. Incontrast, the ortho-P concentrations for Lake Okeechobeebottomsediments increased exponentially with decreasing Eh. Thequantityof NaOH-P fractions for these sediments decreased withdecreasingEh, suggesting the release of Fe- and Mn-bound P intosolution.Phosphate-uptake by Okeechobee bottom sediments (pH 7.5,ambient)followed first order kinetics, yielding a rate constant (k)of 0.51 ± 0.05 h-1. Unlike that of Apopka, the mudsediments in Lake Okeechobee have strong affinity for P ineitheraerobic or anaerobic conditions. Results suggest that even incalcareous systems, Fe and Al, when present in highconcentrations(as in the case of Lake Okeechobee), are actively involved inregulating P-uptake and geochemistry.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...