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Articles containing the keyword 'cation exchange'

Category : Article

article id 5120, category Article
Pentti Sepponen. (1981). Kivennäismaan raekoon tunnuksista ja niiden käyttökelpoisuudesta eräiden maan ominaisuuksien kuvaamiseen. Silva Fennica vol. 15 no. 2 article id 5120. https://doi.org/10.14214/sf.a15061
English title: Particle size distribution characteristics of mineral soil and their applicability for describing some soil properties.
Original keywords: metsämaa; maaperä; lajitekoostumut; raekoko; kenttäkapasiteetti; kationinvaihtokapasiteetti
English keywords: forest soil; particle size distribution; field capacity; degree of sorting; cation exchange capacity
Abstract | View details | Full text in PDF | Author Info

The particle size distribution affects several properties of the soil, thus, the ability to define the texture type of the soil as accurately as possible in field conditions is essential. The soil particle size classification devised by Atterberg (1912) is used in Finnish forestry. The study is based on a small laboratory material. The correlation between some characteristics of the soil particle size distribution, field capacity and cation exchange capacity were determined.

The particle size characteristics such as the relative proportion of different particle sizes, average particle size (Md) and parameters depicting the degree of sorting were determined. The relative proportion of soil particles below 0.06 mm correlated best with both field capacity and cation exchange capacity. Similarly, the average particle size and the degree of sorting correlated well with the field capacity and the cation exchange capacity.

The use of sorting characteristics is not well-suited to the type of soil sample material containing a high proportion of particles of varying size as was used in this material. Such characteristics are probably more easily applicable to the fine sand and sand sediments which are predominant in Finnish forest soils. The most useful particle size distribution characteristics in soils having a great variation in particle sizes were the average particle size and the relative proportion of silt and clay. Thus, the nutrient and water status of the soil can be predicted to some extent by examining the percentage of silt and clay, average particle size and the degree of sorting.

The PDF includes a summary in English.

  • Sepponen, E-mail: ps@mm.unknown (email)

Category : Article

article id 7522, category Article
Timo Kareinen, Ari Nissinen, Hannu Ilvesniemi. (1998). Analysis of forest soil chemistry and hydrology with a dynamic model ACIDIC. Acta Forestalia Fennica no. 262 article id 7522. https://doi.org/10.14214/aff.7522
Keywords: simulation; modelling; aluminium; leaching; water flow; cation exchange; macropores; micropores; flow paths
Abstract | View details | Full text in PDF | Author Info

In this study we analyse how the ion concentrations in forest soil solution are determined by hydrological and biogeochemical processes. A dynamic mode ACIDIC was developed, including processes common to dynamic soil acidification models. The model treats one to eight interacting layers and simulates soil hydrology, transpiration, root water and nutrient uptake, cation exchange, dissolutions and reaction of Al hydroxides in solution, and the formation of carbonic acid and its dissociation products. It includes also a possibility to a simultaneous use of preferential and matrix flow paths, enabling the throughfall water to enter the deeper soil layers in macropores without first reacting with the upper layers. Three different combinations of routing the throughfall water via macro- and micropores through the soil profile is presented. The large vertical gradient in the observed total charge was simulated successfully. According to the simulations, gradient is mostly caused by differences in the intensity of water uptake, sulphate adsorption and organic anion retention at the various depths. The temporal variations in Ca and Mg concentrations were simulated fairly well in all soil layers. For H+, Al and K there were much more variation in the observed than in the simulated concentrations. Flow in macropores is a possible explanation for the apparent disequilibrium of the cation exchange for H+ ad K, as the solution H+ and K concentrations have great vertical gradients in soil. The amount of exchangeable H+ increased in O and E horizons and decreased in the Bs1 and Bs2 horizons, the net change in whole soil profile being a decrease. A large part of the decrease of the exchangeable H+ in the illuvial B horizon was caused by sulphate adsorption. The model produces soil water amounts and solution ion concentrations which are comparable to the measured values, and it can be used in both hydrological and chemical studies of soils.

  • Kareinen, E-mail: tk@mm.unknown (email)
  • Nissinen, E-mail: an@mm.unknown
  • Ilvesniemi, E-mail: hi@mm.unknown
article id 7631, category Article
Carl Johan Westman. (1983). Taimitarhamaiden fysikaalisia ja kemiallisia ominaisuuksia sekä niiden suhde orgaanisen aineksen määrään. Acta Forestalia Fennica no. 184 article id 7631. https://doi.org/10.14214/aff.7631
English title: Physical and physio-chemical properties of forest tree nursery soils and their relation to the amount of organic matter.
Original keywords: viljavuus; taimitarhat; turve; maa; kationinvaihtokapasiteetti; kasvualusta; orgaaninen aines; vedenpidätyskyky
English keywords: peat; soil density; soil; substrate; fertility; nurseries; cation exchange capacity; organic matter; water retention capacity
Abstract | View details | Full text in PDF | Author Info

The aims of the present study were to determine physical and physio-chemical properties of some Finnish forest tree nursery soils, and to examine relationships between these properties and the amount of organic matter in the soil.

The following soil tillage layer properties of 33 fields belonging to 8 forest tree nurseries were determined: soil particle size distribution, organic matter content, bulk density and density of solids, total pore space, soil water volume at potentials pF 2.0 and 4.2, available water content and air space at potential pF 2.0, active acidity, electrical conductivity index and cation exchange capacities at pH 4.5 and 8.0. The soil texture class of the tillage layer parent material was sand, only in a few cases did higher percentage of silt and clay indicate a morainic nature of parent material. The amount of organic material in the soils varied within wide limits, reflecting differences in amelioration policy between the single nurseries.

Relationships between the physical properties of the soil parent material and those related to fertility were in most cases strongly influenced by the amount of soil organic matter. Soil density values decreased as the organic matter content increased from 2 to 25%, giving rise to the increase in the total pore space. However, the amount of water held at potential pF 2.0 and the available water content did not increase with increasing organic matter content. This was due to the absence of the particle fraction in the sand. Nursery soil amelioration, involving in most cases a mixture of Sphagnum peat with sand, thus gives rise to an increase in the content of drainable water.

Cation exchange capacities were positively correlated with the organic matter content. However, the absolute number of exchange sites expressed as equivalents in the tillage layer did not increase in accordance with the increase in organic matter content due to the influence of the organic matter content upon the ratio of solids in the voids.

The PDF includes a summary in English.

  • Westman, E-mail: cw@mm.unknown (email)

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