摘要
在对秦始皇陵开展了汞量测量试验研究中,上方在陵墓发现了高强度的汞异常区,表明深部确有汞源存在,异常范围可能反映了地宫的大体平面位置。热释汞研究证明秦始皇陵上方土壤汞基本由低温汞组成,实际上土壤汞测量是低温汞特征的反映。壤中气汞与土壤汞比较两者具有一致性,相比而言土壤汞更稳定。α杯氡测量在勘查地下汞源和确定陪葬坑的位置等试验中取得初步效果。
In the tentative mercurometric survey around the Qin Shi Huang Tomb, a high mercury anomalous area was detected over the tomb. This suggests that there does exist a mercury source at the depth, and that the area of the mercury anomaly might reflect the approximate position of the underground palace. The heat-release mercury study demonstrates that the soil mercury over the Qin Shi Huang Tomb is basically composed of low - temperature mercury, and that soil survey measurement is actually the reflection of lowtemperature mercury. The volatile mercury in soil is consistent with the soil mercury; nevertheless, the soil mercury is more stable. The α-cup radon measurement has yielded preliminary results in the detection of underground mercury source and the locating of subordinate funeral pits.
出处
《物探与化探》
CAS
CSCD
2005年第4期336-341,共6页
Geophysical and Geochemical Exploration
基金
国家"863计划"项目子课题(2002AA132012)资助
关键词
地球化学勘查
汞量测量
α杯氡测量
秦始皇陵考古
geochemical exploration
mercurometric survey
α-cup radon measurement
archeological study of the Qin Shi Huang Tomb
