FACTORS ON AGRICULTURAL VARY WITH SCALE? Essay, Research Paper
The location of agriculture at all scales is the result of the interaction between physical, cultural and economic and behavioural factors.
Farming in Great Britain has been characterized by technological changes in recent decades which has led to massive increases in yields and improved stock rearing. Much of this change is due to the application of scientific research in plant and stock breeding and improved mechanization. But even today agriculture relies heavily on the physical environment. All crops require a specific range of temperature, moisture, soil ands drainage conditions and these factors can be modified by the farmer but only to a limited degree.
If we accept that a farmers choice of land usage is controlled by the physical environment, we must identify the optimum conditions and limits to production of any one crop . This will help to identify the spatial pattern of environmental controls. This was central to the ideas explored by McCarty and Lindberg in the Mid West of the USA and gave rise to the Optima Limits Model in 1966. Away from the optimum physical conditions become hostile and production/ yields decline. The optimum is the area where yields are highest and variability best, where soils are fertile, temperature and rainfall ideal and ground surface level for cultivation.
Farmers will take account of physical conditions at a local scale when considering which crops to grow. For example, the Moray coast in NE Scotland between Elgin and Lossiemouth is a rich agricultural area where winters are relatively mild and summers averaging 17oC, rainfall occurs throughout the year and is typically 600mm. There are a variety of soils but mainly glacial sandy loams on the higher ground and alluvial soils where there were once areas of open marshy conditions.
A variety of crops are grown, both cereal and root crops. However, there are limitations to agriculture in this area. The main problem is that of wind erosion, the sandy loams are light soils which dry out quickly with high infiltration rates. During early spring or late autumn strong winds can pick up the soil and cause localized wind erosion. Despite this being a well-known problem there are few conservation measures; the only evidence being improving the structure of the soil using manure. There have been no attempts to re-establish hedgerows.
Wetness limitations occur such as at Plewlands Farm to the north of Gordonstoun and at Begrow Farm to the west towards Hopeman. At Plewlands, the wetness means that either rough grazing or root crops occur and cereal growing is avoided in the wetter parts. At Begrow Farm the wet areas are given over to horse paddocks.
From this it is clear that farmers should pay special attention to physical limitations before making decisions about landuse.
The sketch map below illustrates further some controlling physical factors:
The next scale at which physical factors impact on farming can be termed the ‘meso scale’. Within the context of the UK this would focus on regional differences, for example, between East Anglia a
If a line is taken north through the Isle of Wight, to the west at least half of the cultivated area is given over to permanent grass, the further west one goes the greater the proportion of grass. Whilst to the east of this line, cereals are far more important. The predominance of grass in the west and cereals in the east are related to physical differences. Grass provides the cheapest fodder crop for cattle and provides grazing in the summer and hay or silage in the winter. Rainfall is heavier in the west [west Wales 1100mm/year] and gives rise to good grass growth hence prevalence of dairying in places like Devon and west Wales. In eastern England, the sowing of cereal crops is much easier than in the west as the date of return to field moisture capacity is much later in the drier east. Excessive moisture content of soils is less, this helps to make cultivation easier.
Modern grain production requires the use of machinery e.g. combines, which cannot be economically employed on the smaller farms in areas of steep slopes such as can be found in south Devon. In contrast, eastern England has more extensive areas of level relief ( e.g. Fenland- Cambridge and Lincolnshire) where farms are larger and where fields have been amalgamated and hedgerows rooted out. Temperatures are generally a few degrees higher in the east than the west during the growing seasons, again, this tends to favour cereals in the east whilst the cooler, moister west is better for livestock and pasture.
The largest ‘macro’ scale is that which occurs on a global scale. The physical factors of most importance in explaining influences on agriculture are temperature differences. These temperature differences are due to variations in incoming solar energy. The global changes from too cold to too hot, too wet to too dry give rise to general large scale changes in agriculture. So that monsoon tropics in Asia where average annual temp. is 25 C, are typically wet rice cultivation areas, dry arid sub- tropical interiors are desert and typically give rise to nomadism. Hot wet equatorial areas with extensive rain forest have in the past supported shifting cultivation. Temperate maritime regions give rise to seasonal climates allowing a variety of crops and livestock rearing and commercial farming to flourish.
At different scales is possible to see the importance of physical factors. At a local scale, variations in soil quality, moisture content and gradient are significant. As the regional scale, rainfall and large scale relief can give rise to sharp differences. At the global scale, temperature appears to be the major controlling factor.
In conclusion, today new technology across the globe is decreasing the influence of physical factors as they can be overcome by irrigation, fertilizers, temperature modification and increasingly biotechnology and genetical engineering. However, drought can and does persist flooding continues and where it does so, we still seem to be under the influence of the physical environment.
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