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  • Kaupenjohann, Martin  (2)
  • Lang, Friederike  (2)
Type of Medium
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Language
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  • 1
    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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  • 2
    In: Journal of Plant Nutrition and Soil Science, Wiley, Vol. 179, No. 2 ( 2016-04), p. 129-135
    Abstract: Phosphorus is one of the major limiting factors of primary productivity in terrestrial ecosystems and, thus, the P demand of plants might be among the most important drivers of soil and ecosystem development. The P cycling in forest ecosystems seems an ideal example to illustrate the concept of ecosystem nutrition. Ecosystem nutrition combines and extents the traditional concepts of nutrient cycling and ecosystem ecology. The major extension is to consider also the loading and unloading of nutrient cycles and the impact of nutrient acquiring and recycling processes on overall ecosystem properties. Ecosystem nutrition aims to integrate nutrient related aspects at different scales and in different ecosystem compartments including all processes, interactions and feedbacks associated with the nutrition of an ecosystem. We review numerous previous studies dealing with P nutrition from this ecosystem nutrition perspective. The available information contributes to the description of basic ecosystem characteristics such as emergence, hierarchy, and robustness. In result, we were able to refine Odum's hypothesis on P nutrition strategies along ecosystem succession to substrate related ecosystem nutrition and development. We hypothesize that at sites rich in mineral‐bound P, plant and microbial communities tend to introduce P from primary minerals into the biogeochemical P cycle (acquiring systems), and hence the tightness of the P cycle is of minor relevance for ecosystem functioning. In contrast, tight P recycling is a crucial emergent property of forest ecosystems established at sites poor in mineral bound P (recycling systems). We conclude that the integration of knowledge on nutrient cycling, soil science, and ecosystem ecology into holistic ecosystem nutrition will provide an entirely new view on soil–plant–microbe interactions.
    Type of Medium: Online Resource
    ISSN: 1436-8730 , 1522-2624
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2016
    detail.hit.zdb_id: 1481142-X
    detail.hit.zdb_id: 1470765-2
    detail.hit.zdb_id: 200063-5
    SSG: 12
    SSG: 13
    Library Location Call Number Volume/Issue/Year Availability
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