首页|大骨节病区土壤元素分布特征及其与病情的关系——以四川省壤塘县为例

大骨节病区土壤元素分布特征及其与病情的关系——以四川省壤塘县为例

DISTRIBUTION OF SOIL ELEMENTS AND ITS RELATIONSHIP WITH KASCHIN-BECK DISEASE IN KBD AFFLICTED REGIONS——A CASE STUDY OF RANGTANG COUNTY, SICHUAN PROVINCE

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为了探讨大骨节病区土壤元素分布特征及其与大骨节病之间的关系,以病情相对严重的四川省壤塘县为研究区域,采集了0~20 cm和20~40 cm自然土壤和耕作土壤样品,测定其机械组成和Se等9种微量元素.深层土壤中Fe2O3、Co、Se等元素及物理性黏粒的含量略高于表层土壤,而Mo等元素及物理性砂粒的含量则在表层土壤中的含量稍高一些.由于当地土壤受人类活动的影响较小,因而土壤剖面或土层之间的元素含量和机械组成并无明显差异(p>0.05).土壤Mo和Se元素的缺乏导致农作物对这两种元素吸收量的减少,进而造成当地人群特别是儿童处于低Se、低Mo营养状态,这与当地大骨节病病情的关系密切.受母岩和成土作用等的共同影响,理化性质相似的化学元素表现出较好的正相关关系,如Fe2O3、Co、Mn之间呈显著正相关(p<0.01),Zn与Cu、Hg也呈显著正相关关系(p<0.01),但是,这些元素与大骨节病临床患病率均无显著相关性(p>0.05).按大骨节病病情严重程度将所涉及到的行政村平均分为四组:Ⅰ病区(n=6,患病率14.02%~19.87%),Ⅱ病区(n=6,患病率24.62%~28.20%),Ⅲ病区(n=6,患病率28.45%~36.26%),Ⅳ病区(n=5,患病率37.30%~53.66%).由于土壤黏粒和Fe2O3对Se的吸附作用,它们在不同病区的分布特征相同,即土壤黏粒、Fe2O3和Se的含量越低,大骨节病的病情越严重.随病情加重土壤Hg含量呈逐步升高的趋势,但在低Se、低Hg条件下两者是否存在相互作用尚需深入研究.
Rangtang County, Sichuan Province where the prevalence rate of Kaschin-Beck disease (KBD) is relatively high and hence was selected as a typical case in this study to explore distribution characteristics of soil elements andits relationship to KBD. Soil samples were collected from two soil layers (0 ~20 cm and 20 ~40 cm) in natural and cultivated fields, separately for analysis of mechanical composition and total concentrations of nine soil elements. Resultsshowed that the subsoil is higher than the topsoil in contents of Fe2O3 , Co, Se and percentage of physical clay, but lowerin contents of Mo and percentage of physical sand. As the local natural soils are less disturbed by human activities, no significant difference was found on the physicochemical properties between different soil layers or soil profiles (p O 0.05 ).The distribution of Mo and Se elements in the soil led to poor crop uptake of the two elements, thus causing the local population, especially children, nutritional deficiency in Se and Mo, which is demonstrated to be closely related to KBD. Affecred by the parent materials and pedogenesis of the soils, Fe2O3, Co and Mn similar in physical and chemical properties, as well as Zn, Cu and Hg all showed a better positive correlation (p < 0.01). However, no significant correlation was observed between these elements and the clinical prevalence of Kaschin-Beck disease. A total of 23 administrative villages involved in this study were divided into four groups by an ascending sequence in terms of clinical prevalence of Kaschin-Beck disease, i.e. Group Ⅰ (n = 6, incidence rate 14.02% ~ 19.87% ), Group Ⅱ (n = 6, incidence rate 24.62% ~ 28.20% ) , Group Ⅲ ( n = 6, incidence rate 28.45%~ 36.26% ) and Group Ⅳ (n = 5 incidence rate 37.30% ~ 53.66% ). Due to the adsorption of Se by soil clay and Fe2O3, which are similar in distribution characteristics, the disease is getting more severe with decreasing soil clay, Fe2O3 and Se content in the soil. The distribution of Hg in soil was just contrary to that of Se. However, no evidence is confirmed that antagonism exists between Se and Hg in soil low in both.

SoilPhysical claySeleniumKaschin-Beck diseaseRangtang County

张宝军、杨林生、王五一、李永华、李海蓉

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中国科学院地理科学与资源研究所,北京100101

南昌大学公共卫生学院,南昌330006

土壤 物理性黏粒 大骨节病 壤塘县

国家自然科学基金国家自然科学基金国家科技支撑课题

40671008409400092007BAI25B01

2011

土壤学报
中国土壤学会

土壤学报

CSTPCDCSCD北大核心
影响因子:2
ISSN:0564-3929
年,卷(期):2011.48(2)
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