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  • 1985-1989  (2)
  • Geography  (2)
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  • 1985-1989  (2)
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  • Geography  (2)
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  • 1
    Online Resource
    Online Resource
    Wiley ; 1988
    In:  Soil Science Society of America Journal Vol. 52, No. 1 ( 1988-01), p. 261-264
    In: Soil Science Society of America Journal, Wiley, Vol. 52, No. 1 ( 1988-01), p. 261-264
    Abstract: “Salt effects” on soil pH are not well‐documented with highly acidic soils in contact with solutions of very low ionic strength ( 〈 1 m M c /L). These dilute, acidic conditions are typical of soil solutions in many forest ecosystems. A wide range of acid forested soils were contacted with very dilute salt solutions to determine effects of low electrolyte concentrations on soil and solution pH under a variety of experimental conditions. In many soils, pH was lowered markedly following addition of dilute salt solutions. In fact, salt effects on pH (i.e., dpH) were greatest at low concentrations of added salts (e.g., between 0 and 0.6 m M c /L of added salt solutions). At least 40% of the variation in dpH among the 19 mineral soils was attributable to soil differences in low‐level concentrations of water soluble electrolytes. Leaching experiments that manipulated electrolytes in soil solution demonstrated that pH could be depressed up to 1 pH‐unit by increasing salt concentrations by as little as 0.3 m M c /L. Significant correlations between low ionic strength and dpH indicated that water‐soluble electrolytes influence pH w , even of unfertilized, acid soils that are very low in concentrations of soluble ions. Measuring pH of forest soils with 0.01 M CaCl 2 is thus preferable to such measurements with water, to mask variations in soil pH that are caused by variations in relatively low concentrations of water‐soluble electrolytes. Results support the contention that variations in electrolyte concentrations in soil solutions on the order of 0.1 to 0.5 m M c /L (due to natural causes or “acid rain”) affect soil‐solution pH, although probably by relatively minor amounts in many or most soils.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1988
    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
    Location Call Number Limitation Availability
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  • 2
    Online Resource
    Online Resource
    Wiley ; 1989
    In:  Soil Science Society of America Journal Vol. 53, No. 4 ( 1989-07), p. 1222-1228
    In: Soil Science Society of America Journal, Wiley, Vol. 53, No. 4 ( 1989-07), p. 1222-1228
    Abstract: Moisture and nutrient conditions are poorly characterized in soils at elevations 〉 1500 m in the southern Appalachian Mountains. In the Black Mountains, high elevation soils are Typic and Lithic Haplumbrepts, with umbric epipedons that are extremely acid, organic‐rich, rocky, and unstable due to the steep slopes. Many of the Umbrepts in the Black Mountains have been disturbed by exploitative logging, repeated wildfires, and depredation by the balsam woolly adelgid ( Adelges piceae Ratzeburg), each of which has caused major fluctuations in C, nutrient, and hydrologic cycles of soils and ecosystems. The objective of this study was to evaluate predictions based on climate, forest disturbance, and soil genesis: that these soils are rarely subjected to low water potential, that soil N mineralization rates are currently high, and that availability of soil nutrient cations is low. A water balance model appropriate for soils with average water‐holding characteristics indicated that, on a 6‐yr recurrence interval, plants deplete soil moisture to 〈 ‐0.2 MPa during low rainfall periods of one‐month duration. High rock contents (about 0.40 m 3 /m 3 of soil volume in 40‐cm depth) limit soil water storage capacity, and make the spruce‐fir forests very dependent on regular rainfall supplies. Soil N appears mineralizable at moderately high rates, as indicated by three soil and plant indices of N availability, whereas plant availability of Ca and Mg appears marginal. Exchangeable Ca and Mg total only 6.4 and 3.4 kmol c /ha, respectively, in the surface 40 cm of mineral soil, low contents that indicate rapid rates of biogeochemical cycling of divalent cations in these ecosystems. The long‐term recovery of these soils from 20th century disturbances depends directly on the dynamics of soil organic matter, due to organic matter's susceptibility to disturbance and to its control over soil moisture and nutrient availability.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1989
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
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