Download Soils in the Humid Tropics and Monsoon Region of Indonesia by Kim H. Tan PDF

By Kim H. Tan

Highlighting the large adjustments in tropical weather, from sizzling and humid to chill and arctic, Soils within the Humid Tropics and Monsoon area of Indonesia explores the weather, soil zones, and altitudinal version in soil formation. the writer explores the alterations in geomorphology, specifically in weather and crops above sea point, that experience yielded zones of alternative soils.

The booklet makes obtainable hard-to-find info translated from Dutch records. Informally divided into components, it starts with assurance of the advance of soil technological know-how in Indonesia. the writer studies the geography and geomorphology of the archipelago, weather, plants, and mineralization and humification methods as components of soil formation. the second one half examines the most important soils, their genesis, homes, taxonomy, land use, and assessment. The dialogue strikes from lowlands, to uplands, then mountains, and concludes with andosols present in the mountains in addition to within the lowlands.

Focused and well timed, this publication knits new wisdom with outdated yet very important details that has been formerly tough to entry. those gains and extra make it an enormous source during this box.

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Extra info for Soils in the Humid Tropics and Monsoon Region of Indonesia

Example text

A second well-known island is Sumatra, followed by Kalimantan, Sulawesi, Maluku, Nusa Tenggara, and Papua. 1 Geomorphological features of Java Java is approximately 1000 km long and 200 km in width at the widest spots in the western and eastern parts of the island, but it is only 120 km wide at the central part. It is the smallest of the three main western islands of the Sunda Shelf. 1). East of Semarang is found the hilly lands of Rembang, composed of a series of west–east trending ridges, alternating with alluvial plains.

The soils in Indonesia were studied primarily by Dutch scientists, familiar with agricultural conditions in temperate region zones. Soon, it became apparent that these experiences, and in particular those imported from the Netherlands, were not appropriate for applications in situations such as that in Indonesia, if and when not modified appropriately. The need for better scientific soil investigations was stimulated by the necessity to furnish more data, primarily for the thriving Dutch agricultural enterprises or plantations.

Moreover, the purpose is to provide some background information on the geologic materials of importance as parent materials when reading the chapters about soils and soil formation. For those interested in more details about the geology of Indonesia, reference is made to the comprehensive work by van Bemmelen (1949), Brouwer (1922, 1925), Rutten (1927, 1946), and Umbgrove (1938, 1949). In addition to the discussions based on their original investigations, the authors stated above have also compiled almost all the work that has been published by other authors.

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