Summary The processes controlling the retention and release of aluminium in acid forest soils are still subject to controversy, and therefore a universal hypothesis as to what mechanisms are operating has not been firmly established. By studying the Bs horizons of Swedish and Swiss podzolized soils, and by analysing data in the literature, we have found that aluminium hydroxide, and in some cases also poorly ordered imogolite, may control Al solubility in moderately acid (pH > 4.2–4.3) Bs horizons. The strongest evidence in support of the presence of a quickly reacting Al(OH)3 pool came from the temperature dependence of Al solubility in a Bs horizon, which was consistent with the reaction enthalpy of an Al(OH)3 phase such as gibbsite, and from the observation that the ion activity product for Al(OH)3 was the same regardless of whether equilibrium was reached from over‐ or undersaturation. The pool of Al(OH)3 is commonly small and may be completely dissolved after large additions of acid. This may be explained by the continuing redissolution of reactive Al(OH)3 to form less soluble imogolite‐type phases. By using the same methods it was found that soil suspensions did not reach equilibrium with poorly ordered imogolite even after 17 days. Thus, imogolite probably does not control Al solubility in the short term in many soils despite the common occurrence of this mineral. This is due to the relatively slow kinetics of imogolite formation and dissolution, especially at low temperatures and at small solution H4SiO4 concentrations.

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An increasing number of scrapie cases with atypical characteristics, designated Nor98, have recently been recognized. Here, the proteinase K (PK)-resistant prion protein (PrP) fragments from two Swedish cases of Nor98 atypical scrapie have been characterized. The prominent, fast-migrating band in the distinct Nor98 Western immunoblot electrophoretic profile was determined to be of 7 kDa in size and was accordingly designated Nor98-PrP7. The antigenic composition of Nor98-PrP7, as assayed by a panel of anti-PrP antibodies, revealed that this fragment comprised a mid-region of PrP from around aa 85 to 148. N-and C-terminally truncated fragments spanning the mid-region of PrP have only been observed in the genetic prion disorder Gerstmann-Strä ussler-Scheinker disease. It is shown here that the long-term PK resistance of Nor98-PrP7 is reduced compared with that of PrP res in classical scrapie. Enzymic deglycosylation did not change the distinct electrophoretic profile of Nor98-PrP7. A previously unidentified, PK-resistant, C-terminal PrP fragment of around 24 kDa was detected and its PK resistance was investigated. After deglycosylation, this fragment migrated as a 14 kDa polypeptide and was designated PrP-CTF14. Antigenic determination and the size of 14 kDa suggested a fragment spanning approximately aa 120-233. The existence of two PK-resistant PrP fragments, Nor98-PrP7 and PrP-CTF14, that share an overlapping region suggests that at least two distinct PrP conformers with different PK-resistant cores are present in brain extracts from Nor98-affected sheep. The structural gene of PrP in three Nor98-affected sheep was analysed, but no mutations were found that could be correlated to the aberrant PK-resistant profile observed.

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The study was conducted to investigate the relationship between some standard measures of soil reserve potassium (K) and soil mineralogy. Eight different agricultural soils from the N temperate and S boreal regions were studied and analyzed both by standard methods (exchangeable K, 2 M HCl‐ and aqua regia–extractable K) and by quantitative mineralogical methods based on X‐ray powder diffraction analysis of spray‐dried bulk soils. Linear regression and multivariate methods were used to assess the relationships between standard measures of soil reserve K and a number of soil chemical, physical, and mineralogical properties. A mineralogical budgeting approach, to estimate total K and its speciation between different mineral phases, is shown to be accurate after validation against total K analyzed geochemically. This approach enabled us to determine that both HCl‐ and aqua regia–extractable K were highly correlated with K in dioctahedral phyllosilicates and extracted 1%–17% and 5%–45% of total K, respectively. Neither extraction showed any obvious relationship to K in feldspar, which is frequently a larger reservoir of K in the soils examined.

Fifteen Swedish and Finnish soil samples from spodic B horizons containing imogolite-type materials were equilibrated with dilute NaCl and HC1 at 8°C. For the NaCl extracts, apparent equilibrium with respect to an AI(OH)3 phase was reached in one to two weeks. Equilibrium with respect to an imogolite-type phase was slower, especially at large soil:solution ratios. The results show that log *Ks (gibbsite), i.e. the logarithm of the solubility constant for reactive AI(OH)3 at 8°C was ~9.40 (8.29 at 25°C) while log *Ks (imogolite) was variable; for the soil studied in most detail it was 7.66 (6.64 at 25°C) As well-ordered gibbsite rarely forms in spodic B horizons, it is suggested that Al(OH)3 and poorly-ordered allophanic materials may be slowly converted to less soluble and less reactive imogolite-type materials.

The oxyntic mucosa of the human stomach harbors at least five different endocrine cell types (ECL cells, A-like or X cells, somatostatin cells (D), enterochromaffin (EC) cells, and D1 or P cells). Little is known about their functional roles, and of the hormones they produce only somatostatin has been identified. The relative frequency and regional distribution of the different endocrine cell populations were studied in 13 adults with no manifest gastrointestinal disease. From each of them at least three biopsy specimens were taken at seven fixed locations within the oxyntic mucosa. The specimens were examined for the different endocrine cell types by means of immunocytochemistry (staining with antisera against chromogranin A,5-hydroxytryptamine, and somatostatin) and silver staining techniques (demonstration of argyrophil cells by the methods of Grimelius or Sevier-Munger). Chromogranin-positive cells included all endocrine cells identified by the other staining techniques. Grimelius-positive cells included all endocrine cells except the somatostatin cells. Sevier-Munger-positive cells, finally, included the ECL cells and the EC cells. The frequency of ECL cells could be calculated by subtracting the number of EC cells from the number of Sevier-Munger-positive cells. The ECL cells represented 35% of the total endocrine number, somatostatin cells 26%, and EC cells 25%. The remaining 14% consisted of A-like cells, D1 cells, and P cells. Generally, the endocrine cells predominated in the basal portion of the glands, but the various populations of endocrine cells were not uniformly distributed in the various regions of the oxyntic mucosa. However, representative specimens could be obtained from the main body of the stomach, and the results indicate that the examination of a fairly small number of specimens from the main body of the stomach may be sufficient for assessing the frequency of endocrine cells in the oxyntic mucosa of individual patients.

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