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确定^137Cs背景值所需的采样点数与采样面积 被引量:3

SAMPLING NUMBERS AND AREA FOR THE CONFIRMATION OF ^(137)Cs REFERENCE INVENTORY
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摘要 137Cs背景值的确定是利用核示踪技术研究土壤侵蚀的前提和根本,直接关系到侵蚀速率计算的准确与否。而大部分研究对137Cs背景值的确定均采取随机采样,没有统一的采样点数与确定的采样面积。本研究利用网格加密采样法,对未扰动地和长期耕种且未平整的农耕地各两块样地的137Cs背景值空间变异进行了分析,结果表明:在未扰动地与农耕地采样地块,137Cs采样点数与背景值空间变异系数都存在指数回归关系;在未扰动地块137Cs背景值存在较大空间变异性,且随着网格面积的扩大137Cs空间变异系数表现为增加趋势,在0.25m2范围内选取最少11个样点才能满足试验精度;在农耕地采样地块,因长期的耕种作用使得137Cs在耕层中混合相对均匀,137Cs背景值空间变异性显著变小,最少选取7个样点就能满足试验精度,且不受采样面积的影响。 Confirmation of the ^137 Cs reference inventory is the premise and foundation of using ^137 Cs technique to study soil erosion. However, most investigators made the ^137 Cs reference inventory using haphazard approach and lacked the uniform sampling numbers and sampling area. The sampling method of gradually increased grid density was used to study the spatial variation of ^137 Cs reference inventory on undisturbed land and cultivated land in this paper. The results indicated that ^137 Cs inventory showed spatial variation greatly on the undisturbed area. The exponential regression appeared between the number of reference points and CV. With the increasing of grid area, the coefficient of variation of ^137 Cs content displayed the increased trend. And to satisfy the required accuracy of experiment, at least 11 points should be sampled in the area of 0.25m^2. However, due to long-term cultivation on crop land, the ^137 Cs content was mixed uniformly within the plough layer, and the spatial variation decreased obviously. The sampling numbers Of reference points had also the exponential regression relationship with CV. At least 7 points should be sampled to reach accuracy of experiment, and the sampling numbers were not affected by sampling area.
出处 《核农学报》 CAS CSCD 北大核心 2009年第3期482-486,共5页 Journal of Nuclear Agricultural Sciences
基金 国家科技支撑计划(2006BAD09B05) 教育部“新世纪优秀人才”支持计划
关键词 ^137Cs背景值 网格采样 空间变异 ^137 Cs reference inventory grid sampling spatial variability
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参考文献14

  • 1王晓燕,田均良,刘普灵,杨明义.^(137)Cs示踪法研究坡度与土壤流失的关系[J].核农学报,2004,18(5):390-393. 被引量:10
  • 2文安邦,张信宝,沃林DE.黄土丘陵区小流域泥沙来源及其动态变化的^(137)Cs法研究[J].地理学报,1998,53(B12):124-133. 被引量:22
  • 3Ming-Yi Yang,Jun-Liang Tian,Puling Liu.Investigating the spatial distribution of soil erosion and deposition in a small catchment on the Loess Plateau of China,using ^137Cs[J].Soil & Tillage Research,2006,87:186-193
  • 4严平,董光荣,张信宝,邹学勇.青海共和盆地土壤风蚀的^(137)Cs法研究(Ⅰ)——^(137)Cs分布特征[J].中国沙漠,2003,23(3):268-274. 被引量:17
  • 5张春来,邹学勇,董光荣,张信宝,秦芝.干草原地区土壤^(137)Cs沉积特征[J].科学通报,2002,47(3):221-225. 被引量:29
  • 6Theocharopoulos S P,Florou H,Walling D E,Nikolaou T.Soil erosion and deposition rates in a cultivated catchment area in central Greece,estimated using the ^137Cs technique[J].Soil & Tillage Research,2003,69:153-162
  • 7Ross A.Sutherland.Caesium-137 soil sampling and inventory variability in reference localions:A literature survey[J].Hydrological processes,1996,10:43-53
  • 8Basher L R.Matthews K M.Relationship between ^137Cs in some disturbed New Zealand mils and rainfall[J].Australian Journal of Soil Research,1993,31:655-663
  • 9Harper R J,Gilkes R J.Evaluation of the ^137Cs techniques for estimating wind erosion losses for some sandy Western Australian soils[J].Australian Journal of Soil Research,1994,32:1369-1387
  • 10Chisto Takenaka,Yuichi Onda,Yasunori Hamajima.Distribution of cesium-137 in Japanese forest soils:Correlation with the contents of organic carbon[J].The Science of the Total Environmental,1998,222:193-199

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