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  • 1
    In: Biogeosciences, Copernicus GmbH, Vol. 16, No. 7 ( 2019-04-05), p. 1411-1432
    Abstract: Abstract. Dissolved organic matter (DOM) is part of the biogeochemical cycles of carbon and nutrients, carries pollutants and drives soil formation. The DOM concentration and properties along the water flow path through forest ecosystems depend on its sampling location and transformation processes. To improve our understanding of the effects of forest management, especially tree species selection and management intensity, on DOM concentrations and properties of samples from different ecosystem fluxes, we studied throughfall, stemflow, litter leachate and mineral soil solution at 26 forest sites in the three regions of the German Biodiversity Exploratories. We covered forest stands with three management categories (coniferous, deciduous age class and unmanaged beech forests). In water samples from these forests, we monitored DOC concentrations over 4 years and characterized the quality of DOM with UV-vis absorption, fluorescence spectroscopy combined with parallel factor analysis (PARAFAC) and Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR-MS). Additionally, we performed incubation-based biodegradation assays. Multivariate statistics revealed strong significant effects of ecosystem fluxes and smaller effects of main tree species on DOM quality. Coniferous forests differed from deciduous forests by showing larger DOC concentrations, more lignin- and protein-like molecules, and fewer tannin-like molecules in throughfall, stemflow, and litter leachate. Cluster analysis of FT-ICR-MS data indicated that DOM compositions, which varied in aboveground samples depending on tree species, become aligned in mineral soil. This alignment of DOM composition along the water flow path in mineral soil is likely caused by microbial production and consumption of DOM in combination with its interaction with the solid phase, producing a characteristic pattern of organic compounds in forest mineral soils. We found similarly pronounced effects of ecosystem fluxes on the biodegradability of DOM, but surprisingly no differences between deciduous and coniferous forests. Forest management intensity, mainly determined by biomass extraction, contribution of species, which are not site-adapted, and deadwood mass, did not influence DOC concentrations, DOM composition and properties significantly.
    Type of Medium: Online Resource
    ISSN: 1726-4189
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2019
    detail.hit.zdb_id: 2158181-2
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  • 2
    In: Agriculture, Ecosystems & Environment, Elsevier BV, Vol. 265 ( 2018-10), p. 340-349
    Type of Medium: Online Resource
    ISSN: 0167-8809
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2018
    detail.hit.zdb_id: 2013743-6
    SSG: 12
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  • 3
    Online Resource
    Online Resource
    Wiley ; 2003
    In:  Soil Science Society of America Journal Vol. 67, No. 3 ( 2003), p. 795-
    In: Soil Science Society of America Journal, Wiley, Vol. 67, No. 3 ( 2003), p. 795-
    Type of Medium: Online Resource
    ISSN: 1435-0661
    Language: English
    Publisher: Wiley
    Publication Date: 2003
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
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  • 4
    Online Resource
    Online Resource
    Elsevier BV ; 2003
    In:  Geoderma Vol. 113, No. 3-4 ( 2003-5), p. 253-271
    In: Geoderma, Elsevier BV, Vol. 113, No. 3-4 ( 2003-5), p. 253-271
    Type of Medium: Online Resource
    ISSN: 0016-7061
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2003
    detail.hit.zdb_id: 281080-3
    detail.hit.zdb_id: 2001729-7
    SSG: 13
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  • 5
    Online Resource
    Online Resource
    Wiley ; 2003
    In:  Soil Science Society of America Journal Vol. 67, No. 3 ( 2003-05), p. 795-797
    In: Soil Science Society of America Journal, Wiley, Vol. 67, No. 3 ( 2003-05), p. 795-797
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2003
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
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  • 6
    Online Resource
    Online Resource
    Wiley ; 2004
    In:  Soil Science Society of America Journal Vol. 68, No. 4 ( 2004-07), p. 1191-1196
    In: Soil Science Society of America Journal, Wiley, Vol. 68, No. 4 ( 2004-07), p. 1191-1196
    Abstract: To identify the most suitable technique for measuring solute leaching in a sandy soil, we compared three methods in an irrigation experiment (irrigation rates: 5 and 2.4 mm h −1 ) using Cl − as a tracer. We tested tensiometer‐controlled suction plates, wick samplers, and ion‐exchange resin boxes installed between fiberglass pads. Ten samplers of each type were installed at a 52‐cm depth (suction plates) or a 60‐cm depth (wick and resin box samplers) into soil monoliths. The recovery of water and Cl − by the suction plates varied little with irrigation rate (107–118%). The wick samplers performed well during 5 mm h −1 irrigation (Cl − recovery: 111%; water recovery: 103%). However, at the irrigation rate of 2.4 mm h −1 , the water recovery was significantly lower (70%), probably because the soil suction exceeded the maximum capillary force of the wicks. The wicks did not induce a retardation or additional dispersion of Cl − compared with suction plates. The recovery of Cl − by the resin boxes was only 6%. Tensiometer‐controlled suction plates allowed an overall satisfactory estimation of water and solute fluxes in the sandy soil.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2004
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
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  • 7
    Online Resource
    Online Resource
    Wiley ; 2008
    In:  Soil Science Society of America Journal Vol. 72, No. 3 ( 2008-05), p. 786-790
    In: Soil Science Society of America Journal, Wiley, Vol. 72, No. 3 ( 2008-05), p. 786-790
    Abstract: It is unclear whether persulfate digestions completely liberate P associated with mineral colloids in soil solutions and aqueous soil extracts. We tested a modified persulfate digestion using aqueous soil extracts and suspensions of goethite, gibbsite, illite, and montmorillonite that were exposed to 24 μmol P L −1 as orthophosphate (ortho‐P) or myo‐inositol hexaphosphate (IHP). Digestion was performed by autoclaving (121°C, 60 min) 5 mL of extract or suspension after the addition of 1 mL of solution, which contained 150 mmol L −1 K 2 O 8 S 2 and 180 mmol L −1 H 2 SO 4 Subsequently, 0.7 mL of 188 mmol L −1 ascorbic acid was added and the sample was heated in a water bath at 95°C for 60 min. For the samples where P was sorbed onto goethite and gibbsite, recoveries of total P were 97.2 ± 3.7% (ortho‐P) and 102 ± 3.7% (IHP). For the samples where P was sorbed onto clay minerals, average total P recoveries were 99.2 ± 5.1% (ortho‐P) and 106 ± 3.0% (IHP). No differences between total P concentrations measured in persulfate‐digested soil extracts or with an additional digestion with HF and HNO 3 were detected.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2008
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
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  • 8
    Online Resource
    Online Resource
    Wiley ; 2005
    In:  Journal of Environmental Quality Vol. 34, No. 3 ( 2005-05), p. 926-935
    In: Journal of Environmental Quality, Wiley, Vol. 34, No. 3 ( 2005-05), p. 926-935
    Abstract: Fertilization exceeding crop requirements causes an accumulation of phosphorus (P) in soils, which might increase concentrations of dissolved and colloidal P in drainage. We sampled soils classified as Typic Haplorthods from four fertilization experiments to test (i) whether increasing degrees of phosphorus saturation (DPS) increase concentrations of dissolved and colloidal P, and (ii) if critical DPS levels can be defined for P release from these soils. Oxalate‐extractable concentrations of P, iron (Fe), and aluminum (Al) were quantified to characterize DPS. Turbidity, zeta potential, dissolved P, and colloidal P, Fe, Al, and carbon (C) concentrations were determined in water and KCl extracts. While concentrations of dissolved P decreased with increasing depth, concentrations of water‐extractable colloidal P remained constant. In topsoils 28 ± 17% and in subsoils 94 ± 8% of water‐extractable P was bound to colloids. Concentrations of dissolved P increased sharply for DPS 〉 0.1. Colloidal P concentrations increased with increasing DPS because of an additional mobilization of colloids and due to an increase of the colloids P contents. In addition to DPS, ionic strength and Ca 2+ affected the release of colloidal P. Hence, using KCl for extraction improved the relationship between DPS and colloidal P compared with water extraction. Accumulation of P in soils increases not only concentrations of dissolved P but also the risk of colloidal P mobilization. Leaching of colloidal P is potentially important for inputs of P into water bodies because colloidal P as the dominant water‐extractable P fraction in subsoils was released from soils with relatively low DPS.
    Type of Medium: Online Resource
    ISSN: 0047-2425 , 1537-2537
    Language: English
    Publisher: Wiley
    Publication Date: 2005
    detail.hit.zdb_id: 120525-0
    detail.hit.zdb_id: 2050469-X
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  • 9
    In: Journal of Environmental Quality, Wiley, Vol. 39, No. 4 ( 2010-07), p. 1201-1210
    Abstract: The irrigation of agricultural land with wastewater is increasingly practiced in many parts of the world as a consequence of growing populations and urbanization. The risks emerging from pharmaceuticals that are contained in wastewater for soils and groundwater have hardly been investigated. We studied leaching and effects of naproxen, ibuprofen, bezafibrate, diclofenac, gemfibrocil, clarithromycin, trimethoprim, clindamycin, erythromycin, and metoprolol in a soil column experiment simulating an irrigation event with 8.6 cm of wastewater containing 20 μg L −1 or 2000 μg L −1 of each compound or of erythromycin alone. The leached fraction of applied pharmaceuticals ranged from 0.1 ± 0.1% (clarithromycin, 2000 μg L −1 ) to 130 ± 41% (naproxen, 20 μg L −1 ) and tended to increase with decreasing K d or K oc Naproxen transport was similar to that of the tracer chloride. Ibuprofen was also hardly retarded ( R = 1.20 ± 0.18), but showed a higher degradation rate of 0.02 ± 0.004 h −1 (2000 μg L −1 ) than naproxen. The transport of a pulse of 2000 μg L −1 of bezafibrate could be described with a retardation factor of 1.5 and a degradation rate of 0.033 h −1 The application of erythromycin alone or of a cocktail of all pharmaceuticals significantly increased soil CO 2 emissions by 50% 1 d after the application. There is a considerable risk that pharmaceuticals are leached to groundwater during wastewater irrigation.
    Type of Medium: Online Resource
    ISSN: 0047-2425 , 1537-2537
    Language: English
    Publisher: Wiley
    Publication Date: 2010
    detail.hit.zdb_id: 120525-0
    detail.hit.zdb_id: 2050469-X
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  • 10
    Online Resource
    Online Resource
    Wiley ; 2008
    In:  Journal of Environmental Quality Vol. 37, No. 6 ( 2008-11), p. 2100-2107
    In: Journal of Environmental Quality, Wiley, Vol. 37, No. 6 ( 2008-11), p. 2100-2107
    Abstract: The leaching of colloidal phosphorus (P coll ) contributes to P losses from agricultural soils. In an irrigation experiment with undisturbed soil columns, we investigated whether the accumulation of P in soils due to excess P additions enhances the leaching of colloids and P coll from sandy soils. Furthermore, we hypothesized that large concentrations of P coll occur at the onset of leaching events and that P coll mobilized from topsoils is retained in subsoils. Soil columns of different P saturation and depth (0–25 and 0–40 cm) were collected at a former disposal site for liquid manure and at the Thyrow fertilization experiment in northeastern Germany. Concentrations of total dissolved P, P coll , Fe coll , Al coll , optical density, zeta potential, pH, and electrical conductivity of the leachates were determined. Colloidal P concentrations ranged from 0.46 to 10 μmol L −1 and contributed between 1 and 37% to total P leaching. Large P coll concentrations leached from the P‐rich soil of the manure disposal site were rather related to a large P‐content of colloids than to the mobilization of additional colloids. Concentrations of colloids and P coll in leachates from P‐poor and P‐rich columns from Thyrow did not differ significantly. In contrast, accumulation of P in the Werbellin and the Thyrow soil consistently increased dissolved P concentrations to maximum values as high as 300 μmol L −1 We observed no first‐flush of colloids and P coll at the beginning of the leaching event. Concentrations of P coll leached from 40‐cm soil columns were not smaller than those leached from 25‐cm columns. Our results illustrate that an accumulation of P in sandy soils does not necessarily lead to an enhanced leaching of colloids and P coll , because a multitude of factors independent from the P status of soils control the mobility of colloids. In contrast, P accumulation generally increases dissolved P concentrations in noncalcareous soils due to the saturation of the P sorption capacity. This indicates that leaching of dissolved P might be a more widespread environmental problem in areas with P‐saturated sandy soils than leaching of P coll
    Type of Medium: Online Resource
    ISSN: 0047-2425 , 1537-2537
    Language: English
    Publisher: Wiley
    Publication Date: 2008
    detail.hit.zdb_id: 120525-0
    detail.hit.zdb_id: 2050469-X
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