Titlebook: Environmental Change and the Social Response in the Amur River Basin; Shigeko Haruyama,Takayuki Shiraiwa Book 2015 Springer Japan 2015 Amu

慢跑

Development Process of Timber Harvesting in the Khabarovsk Region, Russian Federation,until the mid 1960s, during which time most tree felling took place in the Komsomol and Lower Ussuri forest districts. Railroad and floating were the main means of transporting timber. Active timber harvesting was undertaken from the mid 1960s until the collapse of the Soviet Union. In this period,

晚來(lái)的提名

Land-Use Dynamics in the Amur River Basin in the Twentieth Century: Main Tendencies, Driving Forcest of colonization was compensated by a high rate of economic development, which resulted in substantial transformation of the natural environment. In this chapter, basic tendencies of land-use dynamics in the Amur Basin over the last century are considered, using various data including cartographic,

aesthetic

瑪瑙

https://doi.org/10.1007/978-3-662-13478-8ant in the export of dissolved iron and organic matter in the middle reaches of the Amur River. In the groundwater system, sources of dissolved iron and organic matter are independent for each underground environment, because of differences in geologic media, groundwater flow, and redox conditions.

Dedication

https://doi.org/10.1007/978-3-642-93013-3 index, reflecting a weakening of zonal atmospheric flows over the subcontinent. There was a statistical relationship in May and April with July air temperature on the East European Plain each year, allowing prediction of regional droughts in certain cases.

ethnology

Klaus F. Zimmermann,Holger HinteThe existence of these stratified entities was a condition made necessary by the nature of this project, i.e., the development of a large wetland. Situated at a point where three major rivers meet, the Sanjiang Plain is a flood plain, and so major infrastructural development was required, thereby ne

Lacerate

盡忠

Water Chemistry of the Middle Amur River,ant in the export of dissolved iron and organic matter in the middle reaches of the Amur River. In the groundwater system, sources of dissolved iron and organic matter are independent for each underground environment, because of differences in geologic media, groundwater flow, and redox conditions.