AbstractRare event search experiments using germanium detectors are performed in underground laboratories to minimize the background induced by cosmic rays. However, the cosmogenic activation of cupreous detector components on the ground generates long half-life radioisotopes and contributes to the background level. We measured cosmogenic activation with 142.50 kg of copper bricks after 504 days of exposure at an altitude of 2469.4 m outside the China Jinping Underground Laboratory (CJPL). The specific activities of the cosmogenic nuclides produced in the copper bricks were measured using a low-background germanium gamma-ray spectrometer at CJPL. The production rates at sea level, in units of nuclei/kg/day, were $${18.6 \pm 2.0}$$
18.6
±
2.0
for $${^{54}}$$
54
Mn, $${9.9 \pm 1.3}$$
9.9
±
1.3
for $${^{56}}$$
56
Co, $${48.3 \pm 5.5}$$
48.3
±
5.5
for $${^{57}}$$
57
Co, $${51.8 \pm 2.5}$$
51.8
±
2.5
for $${^{58}}$$
58
Co, and $${39.7 \pm 5.7}$$
39.7
±
5.7
for $${^{60}}$$
60
Co. The measurement will help to constrain cosmogenic background estimation for rare event searches using copper as a detector structure and shielding material. Based on the measured production rates, the impact of the cosmogenic background in cupreous components of germanium detectors on the next generation CDEX-100 experiment was assessed with the expected exposure history above ground.
Source-morphology-independent background estimation for extended gamma-ray sources
