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Please use this identifier to cite or link to this item: http://hdl.handle.net/2239/1680

Title: 强度耕作对~(137)Cs、~(210)Pb_(ex)和有机质剖面分布的影响
Authors: Li, Yong(李勇)
Bai, Lingyu(白玲玉)
Zhang, Xingchang(张兴昌)
Lindstrom M L
Bork H R
Keywords: 137Cs(~(137)cesium (~(137)Cs))
210Pbex(unsupported ~(210)lead ( ~(210)Pb_(ex)))
土壤有机质(soil organic matter)
剖面变异(profile variation)
耕作侵蚀(tillage erosion)
Issue Date: Sep-2003
Publisher: 《水土保持学报》2003,17(3):1-4.
Abstract: [中文摘要]:很少有关于直接测定强度耕作侵蚀引起土壤退化过程的报道。我们的目的是确定应用137Cs和210Pbex直接定量评价耕作侵蚀对土壤有机质(SOM)坡面运移影响的可能性。我们在黄土高原陡坡耕地上进行了50次犁耕活动,并将与其相临的另一块陡坡耕地作为对照。在对照坡地不同坡位,137Cs浓度均匀分布于上部0~30cm土层,而210Pbex浓度在坡上部和坡中部随土层深度增加呈现线性递减,在坡下部呈指数函数递减。0~30cm土层中土壤有机质含量显著大于30cm深度以下土层,并在坡中部和坡下部呈现与210Pbex类似的土壤剖面分布特征。与对照坡地比较,50次犁耕活动导致坡上部、坡中部0~45cm土层的SOM含量分别降低了38%和47%,坡下部0~100cm土层中的SOM含量却提高了18%。坡上部土壤剖面中137Cs浓度的加权平均值从1.48Bq/kg降低到0.29Bq/kg,坡中部从2.53Bq/kg减少到0.33Bq/kg,坡下部从1.48Bq/kg提高到2.81Bq/kg。210Pbex浓度的剖面加权平均值在坡上部从27.71Bq/kg下降到6.15Bq/kg,在坡中部和坡下部分别从35.46Bq/kg和25.53Bq/kg降低到1.57Bq/kg和19.40Bq/kg。137Cs和210Pbex的剖面分布与SOM在p<0.001水平呈显著相关,相关系数R2值在对照坡地为0.81~0.86,在犁耕实验坡地为0.86~0.91。实验结果表明,环境放射性核素137Cs和210Pbex在黄土高原陡坡地遵照同一物理运移机理,可直接应用于定量评价耕作侵蚀与土壤质量的关系。
[英文摘要]:Few direct measurements have conducted to investigate the dynamic process of soil degradation as affected by intensive tillage at the field level. Our objective is to test the potential of 137Cs and 210Pbexfor directly assessing the movement of SOM on the slope land as affected by tillage operations. We conducted 50 plowing operations over a 5day period using a donkeydrawn moldbordplow on steep backslope of the Chinese Loess Plateau. Profile variations of 137Cs, 210Pbex and SOM contents were measured at upper, mid, and lower portion of the slope after 50 plowing operations. Intensive tillage effects on 137Cs, 210Pbex and SOM contents were determined from a control slope adjacent to experimental slope. 137Cs concentration was uniformly mixed in the upper 0~30 cm of soil whereas 210Pbex showed a linear decrease at upper and mid portion, and an exponential decrease with depth on the lower portion of the control slope. SOM contents of 0~30 cm layers were much higher than the soil layers below 30 cm on the control slope, and show ed a similar decrease pattern to profile pattern of 210Pbex on the m id and lower portion of the control slope. Fifty 50-plowing operations resulted in a decrease of SOM content (g/kg) by 38% and by 47% for the soil layers of 0~45 cm at upper portion and mid portion, respectively. How ever, the lower position showed an increase of SOM content by 18% in the soil layers of 0~100 cm after 50 p lowing operations. Weighed mean values of 137Cs concentrations decreased from 1. 48 Bq/kg to 0. 29 Bq/kg at upper position, from 2. 53 Bq/k g to 0. 33 Bq/k g at m id position, and increased from 1. 48 Bq/k g to 2. 81 Bq/kg at lower position. Weighed mean values of 210Pbex concentrations decreased from 27. 71Bq/k g to 6. 15Bq/kg at upper position, from 35. 46Bq/k g to 1. 57Bq/k gatm id position, and from 25. 53 Bq/kg to 19. 40Bq/k gat lower position. Profile concentrations of 137Cs and 210Pbex are significantly correlated with SOM contents with R 2 values of 0. 81~0. 86 for control slope, and 0. 86~0. 91 for experimental slope. Our results suggested that fallout 137Cs and 210Pbex could be used directly for quantifying soil quality-soil redistribution relationship as affected by tillage erosion.
URI: http://seekspace.resip.ac.cn/handle/2239/1680
Appears in Collections:科学论文

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