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Showing items 127 through 135 of 10054.The Kalu Ganga Basin in Sri Lanka is generally flooded once a year. A network of low-lying lands acts as natural retention and storage that captures floodwater, minimizing damage. An increase in the flood frequency has been observed in recent years.
Consolidation and post-consolidation development-related investments are an opportunity to improve living and working conditions of rural residents. Land consolidation is practically the only comprehensive tool to improve the shape of the transport network in the areas covered by this process.
Degraded territory is land which has been damaged by either industrial and other activities or no activities at all to the stage where any economic activity is impossible unless special renewable measures are implemented.
The spatial structure of land in south-eastern Poland is characterized by a high fragmentation, small farms and a road network that is not adjusted to the requirements of modern, mechanized agricultural production.
The aim of article is assessment the impact of the affiliation of the country to the EU-15 or EU-12 on agricultural land productivity and its price.
limatic and hydrological changes will likely be intensified in the Upper Blue Nile (UBN) basin by the effects of global warming. The extent of such effects for representative concentration pathways (RCP) climate scenarios is unknown.
The article presents the main results of investigation of the land market and its problems in Ukraine. Three stages of agricultural land market are singled out and described. The necessity of a moratorium on the sale of agricultural land is present in Ukraine.
The agricultural lands have a special legal regime and are subject to the protection aimed at limiting the seizure of these lands, preserving and increasing their fertility. The area of lands of this category in the structure of land Fund accounts for 100.8 million hа, or 38.6% of used land.
Soil erosion is a very critical form of land degradation resulting in the loss of soil nutrients and downstream sedimentation of water storages in the highlands of Ethiopia.