Yoshikazu Takaya
Biographic Data
| ID | 747474 |
|---|---|
| NAME | Yoshikazu Takaya |
| GIVEN NAMES | Yoshikazu |
| FAMILY NAME | Takaya |
| SIGNATURE | TAKAYA Y |
| AFFILIATIONS | Center for Southeast Asian Studies, Kyoto University |
| VERIFIED | No |
| TOTAL WORKS | 44 |
| TOTAL CITATIONS | 7 |
| AUTHOR COUNT | 44 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1967 |
| LATEST PUBLICATION YEAR | 1996 |
| H-INDEX | 1 |
The Imagined Community”
The view of the " imagined communit that Benedict Anderson proposed in discussing the formation of the nation -state in Indonesia cannot b considered to be correct in that it overlQoks two points First this region is not the homogeneous entity that Anderson considers it to be since it cQnsists of two world units the Java World and the Maritime Southeast Asia World ( Fig1 ) SecQnd Southeast Asia is a world of pantheism where the force that attract…
Forest and the Sea in the Southeast Asian Maritime World
Forest, Sea and Farm Land in Southeast Asia
People and Settlements in Tropical Lowland, with Special Reference to Their Unstability
Agriculture of Madagascar
Kenneth R. Hall. Maritime Trade and State Development in Early Southeast Asia . Honolulu
Traditional Rice Cultivation on Lombok
Sembalun Bumbung a mountain v 1age in I ombok still Ina tains a traditional node of ricc eUltivation tQgether wi its related ritua Land i8 prepared
Agricultural Development of a Tropical Delta
Agricultural Development of a Tropical Delta
Traditional Life and Its Transformation among the Melayu People on the East Coast of Sumatra
On Sangeang Island
Agricultural Transformation in Manigamuwa, a Village in Dry-zone Sri Lanka
Sago Production in South Sulawesi
Landuse along the Pangkajene River, South Sulawesi
Wet
Thais from the Seas
The Reclamation of the Chao Phraya Delta
There were three gro s of people l ving in the Chao Phraya delta prior to the BQwring treaty They werc sedentary rice growers who broadcast rice on the Old Delta shifting rice growers who transplantcd along the coast a 1d the people of
Agricultural Landscape in the Komering River Basin, South Sumatra
Some Ecological Observations on Rice-Growing in Malaysia
Ecology of Traditional Padi Farming in West Malaysia
West Malaysia is divided into seven padi regions: the west coastal plain, is a large wet-pad{ region, wh{le in the Kedah marginal plain (4) padi is grown only in small mountain valleys. 'The.geographical setting of West Mataysih is briefly described from three stand- ' points, climate, landform and landuse, te previde background information for the
Rice Growing Societies of Asia
Vertical Zoning of Monsoon Asia by Agricultural Landuse
Bascd on ficld werk in Indiu and Nepal, mon$oon Asia is classified into five verticHl zones in terms of agricultura] landuse, The llve zones are, froui low to high altitudc, 1) paddy dominant zone, 2) rri,aize-millet and paddy zone ",ith tropical plants, 3) maize- millet ancl paddy zone without tropical plants, 4) maize Kyoto University NII-Electronic Library Service KyotoUniversity /,g.},il'-.fren-'t , the.rnountain range.In order to describe th…
Rice Cropping Patterns in Southern Asian Delta
This paper aims at finding a set ol' correlations possibly existing betwet'n rice crepping patterns and land formsofdc]taic rcgions in S()uthern Asia where ri('e is planted.The Ganges-Brahmaputra, Chao Phraya, Mekong' and Songkei deltas are studied.I.and forms are scherntttieally categerized into six types, viz,, Flootl Releasing Area, Old T)elta, Fleodplain, ltToung Delta, Constal Zone and Local Swale O'igr. 15).Five rjce cropping
An Ecological Interpretation of Thai History
Central Thailand comprises three ecologically distinctive areas, i.e. the mountain area, the floodplain and the delta, as shown in Fig. 1. These three areas relied on irrigation agriculture making full use of the distributary system of intermountain basins. The mountain area was the main stage for the traditional “Muang” during the period from the 12th to the 14th centuries
III. Environmental Conditions of Three Representative Villages in Central Java
Frameworkof the Island of Java It is a matter of common practiee to subdivide the island of Jttva into threc geographical subregions, namely, "Jest, Central and East Java.The political and adininistrative sub- regions follow this cons,entional demarcation, Although we perccivc that the dryness iti landscape increases as we go farther eastwards on thc islund, thc climatic differencc betweenWest and East Java bears no significtLnc,e.According to th…
A Physiographic Classification of Rice Land in the Mekong Delta
The Mekong delta is divided into seven divisions in terms of physiographic character relating to rice culturc, They are Trans-Bassac Horst, Floodplain, Modern Delta, Coastal Complex, Broad Depression, Plain ofReeds and Wcstern Ceastal Zone, and some of them are further subdfvided.Trans-Bassac Horst is a slightly uplifted geologic block with fiat ground surface, Floodplain is a graven fi11cd up by the Bassac and the Mekong's fluviation.Medern Dclt…
Agricultural Development of a Tropical Delta
An Ecological Interpretation of Thai History
Central Thailand comprises three ecologically distinctive areas, i.e. the mountain area, the floodplain and the delta, as shown in Fig. 1. These three areas relied on irrigation agriculture making full use of the distributary system of intermountain basins. The mountain area was the main stage for the traditional “Muang” during the period from the 12th to the 14th centuries
A Physiographic Classification of Rice Land in the Mekong Delta
The Mekong delta is divided into seven divisions in terms of physiographic character relating to rice culturc, They are Trans-Bassac Horst, Floodplain, Modern Delta, Coastal Complex, Broad Depression, Plain ofReeds and Wcstern Ceastal Zone, and some of them are further subdfvided.Trans-Bassac Horst is a slightly uplifted geologic block with fiat ground surface, Floodplain is a graven fi11cd up by the Bassac and the Mekong's fluviation.Medern Dclt…
Rice Lands in the Upland Hill Regions of Northeast Thailand
Quaternary Outcrops of the Southern Part of the Central Plain of Thailand
Quaternar.vOutcrops of the Southern Part of the
Geological Survey Trips along the Maenam
An Outline of the Upper Cenozoic Deposits in the Chao Phraya Basin, Central Thailand
この論文は国立情報学研究所の学術雑誌公開支援事業により電子化されました
Paddy soil survey in India
Observations of some Pleistocene outcrops in Ceylon
Observations on some Pleistocene outcrops in Cambodia
Observations on some Pleislocene outcrops in Cambodia 10 m above the water level of the Tonle Sap (May 30). 1-viii) 2 km NE of Kompong ChhnangGround surface : Narrow flood plain with a small back swamp.Surface is about 4 m higher than the water level of the Tonle Sap (May 30)
Topographical Analysis of the Southern Basin of the Central Plain, Thailand
Geomorphological setting of the soil sampling sites in India
Geomorphological Setting of Soil Sampling Sites in Ceylon
Black soils in eastern India
rkMr9Top" ca6gee4ederived from basaltic Deccan trap rocks either residually or alluvially (and colluvially)
Two Brackish Clay Beds along the Chao Phraya River of Thailand
Two brackish clay beds of different age are found along the lower reaches of the Chao Phraya River ef Thailand.The older one is from 2 to 6m above M. S. L. forming a terrace surface, with from one outcrop to anether, ranging from clayish to coarse sandy ones.The sediment is usually well indurated
Physiography of Rice Land in the Chao Phraya Basin of Thailand
raised portion near the coast is called the deltaic high, andi the rest is the delta flat.The distribution of the six physiographic regions, and their cross sections, are shown in Figs. 1 and 2. These figures are constructed mainly from two topographic maps of 1 to 50,0oo drawn by USAMS2`' and byRTAMSi8
Rice Lands in the Upland Hill Regions of Northeast Thailand
Quaternary Outcrops of the Southern Part of the Central Plain of Thailand
Quaternar.vOutcrops of the Southern Part of the
Physiography of Rice Land in Peninsular Thailand
Rice land in Peninsular Thailand is categorized into three groups with respect to physiographic environment during the wet season and patterns of cuLtivation.The areas under consideration are the lands en the coast, in the young fan region, and in the old fan-terrace regien.On the coast region rice is grown in silted lagoons and in swales between beach ridges.These low-lying areas are moderately inundated for a considerable part of the year and t…
The Plant Height of Rice in Delta
The rice plants in the deltaic area of the Chao Phraya are classified into eight types, from I to VIII, based on the plant height.Type I occursin a geological depression in the middle of the delta, cal]ed Trough, and is distinc- tively characterized by an extreme]y wide height range, varying from 150 c:m to 400 cm {Figs, 2& 3), Type II covers the Old Delta and has a reasenably widc height range and a rapid lateral change ef plant height (Figs. 2 …
III. Environmental Conditions of Three Representative Villages in Central Java
Frameworkof the Island of Java It is a matter of common practiee to subdivide the island of Jttva into threc geographical subregions, namely, "Jest, Central and East Java.The political and adininistrative sub- regions follow this cons,entional demarcation, Although we perccivc that the dryness iti landscape increases as we go farther eastwards on thc islund, thc climatic differencc betweenWest and East Java bears no significtLnc,e.According to th…
A Physiographic Classification of Rice Land in the Mekong Delta
The Mekong delta is divided into seven divisions in terms of physiographic character relating to rice culturc, They are Trans-Bassac Horst, Floodplain, Modern Delta, Coastal Complex, Broad Depression, Plain ofReeds and Wcstern Ceastal Zone, and some of them are further subdfvided.Trans-Bassac Horst is a slightly uplifted geologic block with fiat ground surface, Floodplain is a graven fi11cd up by the Bassac and the Mekong's fluviation.Medern Dclt…
Fai" and "Bo" Type Rice Culture on the Marginal Plain of Thailand
Map published in 1910 suggests that the marginal zone of the Chao Phraya valley has been occupied by two types of rice culture which originated from two regions having different cultural complexes; one is "Fai" type rice culture origination in intermountain basins to the north, and the other is "Bo" type rice culture possibly connected with the Khorat plateau. The former is characterized by "Fai" (dam) and transplanting, and the latter by "Bo" (f…
Saline Soils in Northeast Thailand
The seiected profiles of saline soils in the vicinity of Khorat, Northeast Thailan(l, are descmbed.(.;eomorpho]ogicul interpretation ef the profiles muke the following points clear regarding the origin of the salt
Distribution of Saline Soils in the Khorat Basin of Thailand
The Khorat 1)asin ot' Northeast Thailand is divisible into five categories with respect to the surface sa]inity:1) elevated greund underlain b}r saline Mesozoic rocks, 2) heavily salt-afi'eeted ]owland, 3) moderately salt-affected lowland, 4) slightly salt-affected lowland, and 5) non-saline.These flve zones a,re shown in Fig. 1.* Ii'paFt'th'ent''o'i iLnnd Il)e"eiopment, Thailand
II. Environmental Conditions of Three Representative Villages in Thailand
Rice Cropping Patterns in Southern Asian Delta
This paper aims at finding a set ol' correlations possibly existing betwet'n rice crepping patterns and land formsofdc]taic rcgions in S()uthern Asia where ri('e is planted.The Ganges-Brahmaputra, Chao Phraya, Mekong' and Songkei deltas are studied.I.and forms are scherntttieally categerized into six types, viz,, Flootl Releasing Area, Old T)elta, Fleodplain, ltToung Delta, Constal Zone and Local Swale O'igr. 15).Five rjce cropping
An Ecological Interpretation of Thai History
Central Thailand comprises three ecologically distinctive areas, i.e. the mountain area, the floodplain and the delta, as shown in Fig. 1. These three areas relied on irrigation agriculture making full use of the distributary system of intermountain basins. The mountain area was the main stage for the traditional “Muang” during the period from the 12th to the 14th centuries
Vertical Zoning of Monsoon Asia by Agricultural Landuse
Bascd on ficld werk in Indiu and Nepal, mon$oon Asia is classified into five verticHl zones in terms of agricultura] landuse, The llve zones are, froui low to high altitudc, 1) paddy dominant zone, 2) rri,aize-millet and paddy zone ",ith tropical plants, 3) maize- millet ancl paddy zone without tropical plants, 4) maize Kyoto University NII-Electronic Library Service KyotoUniversity /,g.},il'-.fren-'t , the.rnountain range.In order to describe th…
Rice Growing Societies of Asia
Geography (15 works) · Geology (14 works) · Hydrology (agriculture (12 works) · Agriculture (10 works) · Archaeology (9 works) · Paleontology (8 works) · Vietnamese History and Culture Studies (8 works) · Delta (7 works) · Southeast Asian Sociopolitical Studies (7 works) · Structural basin (7 works)