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  • Kaupenjohann, Martin  (4)
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  • 1
    Online Resource
    Online Resource
    Wiley ; 2004
    In:  Soil Science Society of America Journal Vol. 68, No. 6 ( 2004-11), p. 1853-1862
    In: Soil Science Society of America Journal, Wiley, Vol. 68, No. 6 ( 2004-11), p. 1853-1862
    Abstract: Recent N 2 adsorption studies have suggested a ‘pore clogging’ effect on mineral soil phases caused by organic matter coatings. For methodological reasons, this pore clogging effect has been studied only after drying. Our hypothesis was that pore clogging is affected by drying of organic coatings. In our study, we used AlOOH, which has been equilibrated with dissolved organic matter (DOM) and polygalacturonic acid [PGA; (C 6 H 8 O 6 ) n ]. To test our hypothesis, we determined the porosity of moist and freeze‐dried AlOOH samples. Freeze‐dried samples were analyzed by N 2 adsorption, moist samples by 1 H‐nuclear magnetic resonance (NMR). In addition, the samples were characterized by environmental scanning electron microscopy—energy dispersive x‐ray spectroscopy (ESEM‐EDX). Both, DOM and PGA significantly reduced specific surface area (SSA BET ) of AlOOH by 34 m 2 g −1 (15%) and 77 m 2 g −1 (36%). The reduction in SSA BET normalized to the amount of C sorbed was 1.0 m 2 mg −1 DOM‐C and 5.9 m 2 mg −1 PGA‐C. Dissolved OM reduced the pore volume of micro‐ and small mesopores 〈 3 nm whereas PGA also reduced the volume of larger pores. The 1 H‐NMR results of moist samples showed that PGA sorption reduced the amount of water in pores 〈 4 nm. In addition, the pore size maximum of AlOOH increased by 150%. Polygalacturonic acid coatings created new interparticle pores of about 10‐ to 70‐nm size that are not stable upon freeze‐drying. Porosity changes upon DOM‐treatment were not commensurable by 1 H‐NMR. Our results indicate that clogging of micro‐ and small mesopores is not an artifact of freeze‐drying. Polygalacturonic acid seems not only to cover the mouth of AlOOH‐nanometer pores but also to fill them.
    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
    Library Location Call Number Volume/Issue/Year Availability
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  • 2
    Online Resource
    Online Resource
    Wiley ; 2006
    In:  Soil Science Society of America Journal Vol. 70, No. 2 ( 2006-03), p. 541-549
    In: Soil Science Society of America Journal, Wiley, Vol. 70, No. 2 ( 2006-03), p. 541-549
    Abstract: Biogenetic polysugars may affect the sorption characteristics of soil mineral particles in the rhizosphere. We hypothesized that polygalacturonate [PGA, (C 6 H 7 O 6 ) n − ] coatings on goethite reduce the diffusion of phosphate into the pores of the adsorbent. Goethite was preloaded with PGA (0–10 mg C g −1 ). The samples were characterized by N 2 and CO 2 adsorption, electrophoretic mobility measurements, and scanning electron microscopy/energy dispersive X‐ray analysis (SEM‐EDX). The phosphate sorption kinetics was studied with batch experiments over 2 wk at pH 5 and an initial phosphate concentration of 250 μ M Pore volume and specific surface area of the goethite samples declined after PGA addition. The PGA coatings reduced the ζ‐potential of goethite from 42.3 to −39.6 mV at the highest C loading. With increasing PGA‐C content and decreasing ζ‐potential the amount of phosphate sorbed after 2 wk decreased linearly ( P 〈 0.001). Sorption of phosphate to pure and PGA‐coated goethite showed an initial fast sorption followed by a slow sorption reaction. At the smallest C loading (5.5 mg C g −1 ) the portion of phosphate retained by the slow reaction was smaller than for the treatment without any PGA, while at higher C loadings the fraction of slowly immobilized phosphate increased. Our results suggest that at low C‐loadings PGA impaired the intraparticle diffusion of phosphate. In contrast, the slow step‐by‐step desorption of PGA ( 〈 52% within 2 wk) or the diffusion of phosphate through PGA coatings or both are rate limiting for the slow phosphate reaction at C loadings 〉 5.5 mg C g −1
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2006
    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
    Library Location Call Number Volume/Issue/Year Availability
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  • 3
    Online Resource
    Online Resource
    Elsevier BV ; 2006
    In:  Geochimica et Cosmochimica Acta Vol. 70, No. 3 ( 2006-2), p. 595-607
    In: Geochimica et Cosmochimica Acta, Elsevier BV, Vol. 70, No. 3 ( 2006-2), p. 595-607
    Type of Medium: Online Resource
    ISSN: 0016-7037
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2006
    detail.hit.zdb_id: 300305-X
    detail.hit.zdb_id: 1483679-8
    SSG: 13
    SSG: 16,12
    Library Location Call Number Volume/Issue/Year Availability
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  • 4
    Online Resource
    Online Resource
    Wiley ; 2006
    In:  Soil Science Society of America Journal Vol. 70, No. 5 ( 2006-09), p. 1547-1555
    In: Soil Science Society of America Journal, Wiley, Vol. 70, No. 5 ( 2006-09), p. 1547-1555
    Abstract: Organic coatings on Fe oxides can decrease the accessibility of intraparticle pores for oxyanions like phosphate. We hypothesized that the slow sorption of phosphate to goethite coated with polygalacturonate (PGA) is controlled by the accessibility of external goethite surfaces to phosphate rather than by diffusion of phosphate into micropores (Ø 〈 2 nm). We studied the phosphate sorption kinetics of pure and PGA‐coated goethites that differed in their microporosity (N 2 at 77 K, 46 vs. 31 mm 3 g −1 ). Because drying may affect the structure or surface coverage of PGA, we also tested the effect of freeze‐drying on the slow phosphate sorption. The samples were examined by gas adsorption (N 2 , CO 2 ) and electrophoretic mobility measurements. Phosphate sorption and PGA‐C desorption were studied in batch experiments for 3 wk at pH 5. In PGA‐coated samples, the slow phosphate sorption was independent of micropore volume. Phosphate displaced on average 57% of PGA‐C within 3 wk. Similar to phosphate sorption, the PGA‐C desorption comprised a rapid initial desorption, which was followed by a slow C desorption. Sorption competition between phosphate and presorbed PGA depended on the 〈 10‐nm porosity and the C loading of the adsorbent. The efficacy of phosphate to desorb PGA generally increased after freeze‐drying. We conclude for PGA‐coated goethites that (i) freeze‐drying biased the slow phosphate sorption by changing the structure/surface coverage of PGA, and (ii) within the time frame studied, micropores did not limit the rate of the slow phosphate sorption. Rather, the slow, gradual desorption of PGA and/or the diffusion of phosphate through PGA coatings controlled the slow phosphate sorption to PGA‐coated goethite.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2006
    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
    Library Location Call Number Volume/Issue/Year Availability
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