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In view of the importance of soil material characteristics in determining paddy soil capability, a method of classification for soil materials was proposed. In working out the method special attention was paid to making it practically applicable, for the need is great for such a method of ready practical applicability especially in the alluvial soil areas in which most Japanese paddy soils occur.

An X-ray fluorescence spectrographic method for the total chemical analysis of soil materials proved satisfactory for routine use in terms of accuracy and time. Nine major elements (Si, Fe, Al, Ca, Mg, Mn, Ti, K, P) were analyzed and they were taken to represent the chemical nature of the soil material. The total chemical composition was combined with mechanical composition and subjected to data processing.

To avoid redundancy in information, 2 mutually independent principal components were extracted, which appear to represent different aspects of soil material features. From the 2 principal component scores taxonomic distance was computed as a similarity coefficient for use in numerical taxonomy.

By means of numerical taxonomy 8 Soil material classes were set up, each of which was characterized in terms of texture, base status, weatherable mineral reserve, etc. In order to facilitate objective placement of a new sample into one of the classes set up, discriminant functions were derived for all pairs of the 8 material classes. A figure showing the discriminant space that corresponds to the discriminant functions was prepared to make the practice of discrimination easy.

The 8 soil material classes appear to represent major varieties of paddy soil materials in Japan. The use of the soil material classes as a basis, of “soil family” separation m soil surveys would improve the homogeneity of the lower taxonomic units (“soil series”) and make their interpretation easier and more correct in relation to soil capability assessment.  相似文献   
23.
Changes in dispersibility and charge characteristics of two soils with different colloidal properties were investigated after various extracting treatments of free oxides. The soil samples were taken from the upland field in a reclaimed area (highly dispersive) and from the B horizon of an adjacent forest area (physically stable), both of which derived from the same parent material. Special attention was paid to selective extraction of Al and Fe oxides. After the extraction of free oxides by conventional methods such as DCB or oxalate treatment, dispersibility of the soils which always became too high made it difficult to relate the amounts of removed oxides with the changes in dispersibility. Thus, extractions by milder treatments were designed in order to remove varying amounts of free oxides using several organic salt solutions. Among the treatments, citrate and oxalate extracted more Al oxides, followed by tartrate. Dithionite, acetate, and NaCl extracted only trace amounts of Al oxides. This order seemed to be controlled by the stability constants of organo-Al complexes. The changes in dispersibility of the residual soil were related to the amount of extracted Al, especially for the forest soil, but not to Fe or Si. After these treatments, the amount of positive charges of the soil decreased while that of negative charges increased. For instance, the amount of total charges of the forest soil after DCB treatment was 1.5 times larger than that of the non-treated soil at the dispersion pH, which was mainly attributed to the removal of Al oxides. Although the amount of removed Al oxides was relatively small, the changes in dispersibility of the residual forest soil were drastic, indicating that free oxides (mainly Al) removed by milder treatments were the most external, active fractions. This interpretation suggests the practical importance of the release of amorphous sesquioxides in the natural weathering process in preventing the dispersion of potentially dispersive soils.  相似文献   
24.
Abstract

A soil map is eonventionally prepared by an experieneed surveyor via the following three steps; (1) establishment of taxonomie class, (2) alloeation of sam pie into one of the classes, and (3) delineation of homogeneous areas in terms of mapping unit. These steps involve some degree of arbitrariness; thus soil maps prepared by two surveyors are never identical. The aim of this study is to define a eertain proeedure of soil map eompilation, by introdueing numerical handling of soil data, to obtain a reproducible and easy-to-prepare soil map, with the help of the funetions of the eomputer-based Soil Data Management System (COSMAS).

The authors applied Hayashi's theory of quantification No. 3 to numerical representation of soil profiles based on the pattern of eombination of various soil attributes relevant to soil classification. The following four soH types were recognized in the seattergram plotted using numerical va lues assigned to the soH profiles; Gley Lowland SoH, Gray Lowland Soil, Brown Lowland Soil and Pseudogley SoH. Then, using these numerical values, diseriminant analysis was carried out to classify each profile into one of the above-defined soil types. As a result, 89.7% of the observed profiles were assigned to the same soil types as assigned by a surveyor in the filed. Area delineation for each mapping unit on the basis of soil type assignment and probabHity of membership of a respective soil type group at a sampled si te was automatieally performed by an "AUTOMAP" program whieh was newly developed for COSMAS for graphic representation of soil data. The numerically prepared soi! map showed reasonable agreement with the surveyor's. A wide range of users of soil survey data can prepare various maps using the procedure proposed in this paper.  相似文献   
25.
26.
“The union of mineral and organic matter to form the organo-mineral complex is a synthesis as vital to the continuance of life as, and less understood than, photosynthesis.”(JACKS) (1).  相似文献   
27.
Clay fractions of three Andosols and a Latosol occurring in Indonesia, and two Alluvial Soils derived from pyroclastic sediments in the Philippines were examined by means of chemical analyses, X-ray diffraction, differential thermal analysis, thermogravimetry, infrared absorption spectroscopy, and electron microscopy. The results are summarized as follows.

Allophane is a dominant clay mineral of young volcanogenous soils occurring in the tropics. Small amounts of halloysite, gibbsite, and imogolite are also found in some of the young volcanogenous soils. Halloysite and imogolite are relatively abundant in the surface soil, while gibbsite is more abundant in the subsoil. In the clay fraction of the young volcanogenous soils in the tropics, α-cristobalite is often present, but quartz occurs rarely. Small amounts of feldspars are also present in the Philippine soils. 2 : 1-type minerals are found to a small extent in some of the sample soils. The above results agree well with the results for Japanese Andosols, except for a difference in the primary mineral composition.  相似文献   
28.
Utilizing the data and materials accumulated in the project “Observations on Soil Fertility Changes” organized by Ministry of Agriculture and Forestry and executed by 16 Prefectural Agricultural Experiment Stations throughout Japan, an attempt was made to derive a prediction equation for soil loss due to erosion.

Five Prefectural Agricultural Experiment Stations provided us with rainfall records from which monthly rainfalls by three intensity grades, under 2 mm/10 min (LE2R), 2-4 mm 10 min (MEDRi) and over 4 mm/10 min (GT4R), were read. Multiple regression of log-transformed soil loss upon these rainfall data gave the following regression equation

Log soil loss = -0.783 0.0185**GT4R+0.00597**LE2R -0.00763**MEDR for which multiple correlation coefficient (R) was 0.74. The units of measurement were kg are for soil loss mm/month for LE2R, MEDR, and GT4R.

In order to account for the contribution of slope and soil factors to soil loss, Hayashi's theory of quantification No. I was applied after coding the relevant data. R of log-transformed soil loss on GT4R, MEDR, LE2R, slope, bulk density (BD), and texture (TEXT), reached 0.80. GT4R had the highest partial correlation coefficient, followed successively by MEDR, slope, and LE2R. Bulk density (BD) and texture (TEXT) were taken from among the data available to represent characters relevant to erosion, but they had onlv low partial correlations with soil loss in this Particular study.

The method developed in this study appears to be promising only if properly collected data are available. Conditions that should be satisfied in the planning of experiments for the purpose derivation of a prediction equation have been put forward.  相似文献   
29.
In 1946 BREMNER et al.(1) suggested a theory that, in soils, polyvalent metals are combined with organic matter as metal-organic matter complexes, and that these complexes are insoluble in solvents that do not themselves form complexes with metals. The principle of one of the most prevailing methods for humus extraction, the neutral sodium pyrophosphate extraction proposed by BREMNER and LEES (2), is a corollary of the theory.  相似文献   
30.
Influence of Al dissolution on soil ZPC (zero point of charge) measured by a potentio-metric titration (PT) method and a modified salt titration (STPT) method was examined using two strongly weathered soils from Thailand and two volcanic ash soils from Japan. The amount of dissolved Al ions increased with the increase in the concentration of a supporting electrolyte for the strongly weathered soils, while the increase was negligible for the volcanic ash soils.

ZPC value of the strongly weathered soils determined by the PT method was lower than that by the STPT method, due to the greater Al dissolution associated with the higher electrolyte concentration used in the PT method. Al ions adsorbed onto the soil surface would shift the ZPC to a higher pH value not as a result of the formation of hydroxy Al polymers, but due to the blocking of permanent negative charge sites, which could otherwise lower the ZPC. The σp value, as a measure of permanent charge or the amount of 11 or O11 adsorbed by a soil required to attain the ZPC, could be used to describe this phenomenon.

In the STPT method, the salt concentration was not high enough to causc a significant Al dissolution at the ZPC, which is considered to be a more suitable condition than in the PT method because the ZPC value can be evaluated at a low salt concentration as in the ease of field conditions for crop production. Thus, the STPT method is rccommendcd for the determination of the ZPC.  相似文献   
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