tee ae DK . a , +, gos ' : :“ Ota! | . ‘ oo . - . oy , . : Moe ; . . . Ms me as . ot : oF 4 . Meet ‘ . . vO s a aan Cote, ‘ ‘ bbe es ea cou wn: RO we . . poe “ah hoe a : - . January 12, 1963) . A RECENT evaluation of radiological data gathcred by the U.S. Atomic Energy Commission's Health and Safety Laboratory includes a statement that the concentration of fission products in commercial milk is essentially independent oftotal rainfall':?. However. the precipitation values were presented as arbitrary ranges and the landscape units used were not strictly biological regions. The purpose of this communication is to show that if radiological data from the same source are arranged according to natural landscape units a relationship between phytoelimatic zones and the ecsxsium-137 content of milk is indicated. . . . . For our purpose, the geographical region considered is the north-western portion of the United States where broad areas are mappedas distinctive natural vegetation zones’. Such broad areas are necessary to allow reasonable assurances that milk sample stations actually derive milk from an area representative of a particular vegetation zone. Ten of eleven milk sampling stations in the north-west region were grouped into one of three natural vegetation zones (Table 1). Portland, Oregon and Burlington. Washington. were assigned to the Pacific north-west coniferous forest zone. Bismarck, Bottineau, and Cando, North Dakota; and Mitchell, South Dakota, were assigned to the grassland zone. Sunnyside, Washington: Payeite and Idaho Falls, Idaho; and Monroe, Utah, were assigned to the sage-brush zone. Because of its proximity to the Wasatch Mountains, which provided a diversity of a eee ‘ 407948 Relation to Phytoclimatic Zones wae? , (Reprinted from Nature, Vol. 197, No. 4863, pp. 197-198. Czsium-!37 in Dried Milk Products in . a. te wo . ee ate . vegetation zones within a small area. the milk sampling station of Ogden, Utah, was excluded. Cexsium-137 is deposited on aerially exposed plant parts directly from the atmosphere and the amounts ingested and assimilated by grazing animals are dominantly from this source rather than from plant uptake via contaminated soils‘. Total precipitation is regarded as important in depositing cesium-137 over landscapes and the amounts deposited are related to the amountof precipitation ; moist regions receive more cesium-137 than regions of less moisture®. The cesium-137 content of milk samples in pe./g potassium from stations grouped according to vegetation zones is presented in Table 1. Milk products from sampling stations in the coniferous zone averaged 90 pc./g potassium as compared with only 54 and 37 for grassland and sagebrush zones. Total precipitation from weather stations fe

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