Volume 12,Issue 1,1964 Table of Contents

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  • 1  THE DISTRIBUTION AND RECLAMATION OF SALINE-ALKALI SOILS OF NORTH CHINA PLAIN AND THE WEI-HO PLAIN IN THE PERIOD OF CHOU-HAN DYNASTIES
    H. J. WEN C. L. LIN
    1964, 12(1):1-9.
    [Abstract](1714) [HTML](0) [PDF 785.85 K](3419)
    Abstract:
    Ancient chronicles recorded that duriag the period of B.C. 1122-A.D. 220 saline-alkali soils occupied large areas along the sea coast of North China Plain. Inland saline-alkali soils were found in the northern part of the Plain, and also in the northern part of the Wei-ho Plain. In that period, amelioration of these soils were accomplished by using good irrigation-drainage system, by leaching, by rice planting and also by silting from periodical flooding water.
    2  МЕЛИОРАТИВНОЕ РАЙОНИРОВАНИЕ И МЕРОПРИЯТИЯ ПО БОРЬБЕ С ЗАСОЛЕНИЕМ ПОЧВ В РАЙОНЕ ЛЯОЧЭНА
    Ван Цзунь-цин Лю Ю-чан Ли Ли-цюнь Дун Чао-пэн
    1964, 12(1):10-22.
    [Abstract](1750) [HTML](0) [PDF 3.20 M](2676)
    Abstract:
    Прн разработке мелиоративного районроваия по борьбе с засолением почв необходимо учитывать как особенность сочетания природных условий, так и особениость сельского хозяйства.
    3  ГЕНЕЗИС И СВОЙСТВА ОСНОВНЫХ ТИПОВ ПОЧВ РАВНИНЫ ИНЬЧУАНЬ И ПУТЬ ИХ МЕЛИОРАЦИИ И ИСПОЛЬЗОВАНИЯ
    Ван Цзе-чжи
    1964, 12(1):23-33.
    [Abstract](2282) [HTML](0) [PDF 798.56 K](2891)
    Abstract:
    Равнина Иньчуань расположена в зоне пустынных степей。Зональными лочвами её являются светлые сероземы, которые распространяются на высших террасах равнины.
    4  СОВРЕМЕННОЕ СОЛЕНАКОПЛЕНИЕ В ГРУНТОВЫХ ВОДАХ И ПОЧВАХ СУНГАРИ-НОННИНСКОЙ РАВНИНЫ
    Ли Чан-хуа
    1964, 12(1):34-42.
    [Abstract](1552) [HTML](0) [PDF 666.60 K](2834)
    Abstract:
    1. К проаинции сульфатно-хлорндпо-содового соленакопления относится Сунгари-ноннинская равнина, расположенная в зоне переходной от лесостепн к степн.
    5  ХАРАКТЕРИСТИКА КЛЕЯЩИХ ВЕЩЕСТВ КРАСНОЗЕМНЫХ И КРАСНОЗЁМОВИДНЫХ РИСОВЫХ ПОЧВ И СВЯЗЬ ИХ С СТРУКТУРООБРАЗОВАНИЕМ ПОЧВ В ЦЕНТРАЛЬНОЙ ЧАСТИ ПРОВИНЦИИ ЦЗЯНСИ
    Яо Сянь-лян Юй Дз-фен
    1964, 12(1):43-54.
    [Abstract](1458) [HTML](0) [PDF 3.00 M](3080)
    Abstract:
    В настоящей статьи изучена связь количества и состава клеящих веществ краснозёмных и краснозёмовидных рисовых почв с их структурообразованием в центральной частн провинции Цзянси путём коллоидно-химического метода и техники микроскопического исследования.
    6  ON THE PROPERTIES OF THE MICRO-AGGREGATES OF PADDY SOILS DERIVED FROM QUARTERNARY RED CLAY
    Q. HO C. F. CHEN
    1964, 12(1):55-62.
    [Abstract](1728) [HTML](0) [PDF 614.04 K](2859)
    Abstract:
    Three groups of micro-aggregate, including water dispersed (G0,sodium dispersed (G1) and mechanical-sodium dispersed micro-aggregate (G2),were separated by the peptization method from three groups of paddy soil derived from Quarternary red clay. The total amounts of micro-aggregates are 54, 58, 60% based on air-dry soil and the ratio of G0+G1:G2 are 0.45, 0.94, 1.46 respectively.
    7  ГЕНЕЗИС И ЭВОЛЮЦИЯ РИСОВЫХ ПОЧВ ЮЖНОГО РАЙОНА ПРОВИНЦИИ ЦЗЯНСУ
    СЮй Чи
    1964, 12(1):64-73.
    [Abstract](1551) [HTML](0) [PDF 2.98 M](2696)
    Abstract:
    Южный район провинции Цзянсу является древнейшим районом земледелия.
    8  ТЕПЛОВОЙ РЕЖИМ ОРОШАЕМОЙ ПОЧВЫ ПОД ПШЕНИЦАМИ
    Шин Лай-цюань
    1964, 12(1):74-77.
    [Abstract](1402) [HTML](0) [PDF 271.74 K](2555)
    Abstract:
    Орошение является важным мероприятием улучшения почвенного климата и повышения урожая с единицы площади.
    9  APPRAISAL OF THE METHODS OF DETERMINING AVAILABLE FORMS OF PHOSPHATE EXTRACTED FROM SOILS
    LI YAO-HUI
    1964, 12(1):78-82.
    [Abstract](1600) [HTML](0) [PDF 382.77 K](2594)
    Abstract:
    The forms of phosphate extracted from soils by various methods were established by calculation according to the law of solubility product. Ammonium carbonate solution may extract water soluble phosphates, CaHPO4·2H2O, CaHPO4, Ca4H(PO4)3·3H2O,aluminum and iron phosphates, a little organic phosphorus and probably a little Ca3(PO4)2, and Ca5(PO4)3OH,similarly sodium carbonate solution may extract the same phosphates except those in organic forms. Sodium citrate solution extracts water soluble phosphates, CaHPO4·2H2O, CaHPO4, aluminum and iron phosphates, and a little organic phosphorus. Lactate solution and Burriel-Hernando's extractant extract all forms of calcium phosphates in soils, but not aluminum and iron phosphates as well as organic phosphorus. Ammonium oxalate solution extracts all the above forms of phosphate from soils.Recovery test made on CaHPO4, Ca3(PO4)2 and FePO4·4H2O confirmed the results from calculation.The difference in the degree of correlation between the available phosphorus content as determined by the various methods and the response of crops to phosphorus fertilization was explained by the forms of phosphate extracted and the present knowledge of their availability.
    10  DETERMINATION OF WATER SOLUBLE POTASSIUM IN SOILS BY TETRAPHENYLBORON Ⅰ. ARGENTOMETRIC AND BROMATOMETRIC METHODS
    Y. K. LI
    1964, 12(1):83-90.
    [Abstract](1889) [HTML](0) [PDF 618.92 K](2703)
    Abstract:
    The present paper deals with the investigation on the argentometric and bromatometric methods for the determination of water soluble potassium with TPB (tetraphenylboron) in saline soils. Modifications of these methods are recommended.In the argentometric titration, the writer recommends the use of fluorescein as an adsorption indicator which gives a better color contrast of yellowish green fluorescence to pink. In addition, this method is comparatively simple and inexpensive.In the bromatometric method instead of the sintered glass filter an ordinary retentive, quantitative filter paper has been found adoptable in filtering the K-TPB precipitate. The bromatometric method, though comoarativelv tedious. gives a higher degree of accuracy and precision than the argentometric method.
    11  DETERMINATION OF NITROGEN IN ORGANIC SUBSTANCES
    KUAN TZE-YAN
    1964, 12(1):91-93.
    [Abstract](2872) [HTML](0) [PDF 218.72 K](2829)
    Abstract:
    A modified oxidation-reduction titration method for the determination of nitrogen in organic matter after Kieldahl dieestion is described. The catalysts includine copper, selenium or mercury, which often interfere with the end point of oxidation-reduction titratIon, were removed by addition of zinc granules.

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