The sensitivity of an experiment to detect the Majorana neutrino mass via neutrinoless double-beta decay(0νββ) strongly depends on the rate of background events that can mimic this decay. One major source of this b...The sensitivity of an experiment to detect the Majorana neutrino mass via neutrinoless double-beta decay(0νββ) strongly depends on the rate of background events that can mimic this decay. One major source of this background is the radioactive emissions from the laboratory environment. In our study, we focused on assessing the background contributions from environmental gamma rays, neutrons, and underground muons to the Jinping bolometric demonstration experiment. This experiment uses an array of lithium molybdate crystal bolometers to probe the potential 0νββ decay of the100Mo isotope at the China Jinping Underground Laboratory. We also evaluated the shielding effectiveness of the experimental setup through an attenuation study. Our simulations indicate that the combined background from environmental gamma rays, neutrons, and muons in the relevant100Mo 0νββ Q-value region can be reduced to approximately 0.003 cts/kg/keV/yr.展开更多
为模拟详细的温度分布信息,进一步理解地表能量平衡过程,提高植被冠层温度反演精度,根据土壤阴影表面和光照表面的热源和蒸发速率的差异,扩展了CU P ID模型,实现了光照和阴影土壤组分温度分布模拟。采用实测数据分别对冬小麦和夏玉米冠...为模拟详细的温度分布信息,进一步理解地表能量平衡过程,提高植被冠层温度反演精度,根据土壤阴影表面和光照表面的热源和蒸发速率的差异,扩展了CU P ID模型,实现了光照和阴影土壤组分温度分布模拟。采用实测数据分别对冬小麦和夏玉米冠层下的土壤组分温度进行了模拟和验证。在冬小麦地,模拟光照和阴影土壤温度绝对差值为2.8 K和2.4K,平均差值为-1.5 K和-0.7 K;在夏玉米地,模拟与实测温度绝对偏差为3.8 K左右,平均偏差为-0.5 K。总体来说,模拟与实测数据吻合较好,说明扩展模型能够较为真实地反映土壤组分温度分布及其变化。扩展模型可在组分温度反演和农业旱情监测等领域得到应用。展开更多
基金supported in part by the State Key Research Development Program in China(Nos.2022YFA1604702 and 2022YFA1604900)the National Natural Science Foundation of China(No.12025501)Strategic Priority Research Program of Chinese Academy of Science(No.XDB34030200).
文摘The sensitivity of an experiment to detect the Majorana neutrino mass via neutrinoless double-beta decay(0νββ) strongly depends on the rate of background events that can mimic this decay. One major source of this background is the radioactive emissions from the laboratory environment. In our study, we focused on assessing the background contributions from environmental gamma rays, neutrons, and underground muons to the Jinping bolometric demonstration experiment. This experiment uses an array of lithium molybdate crystal bolometers to probe the potential 0νββ decay of the100Mo isotope at the China Jinping Underground Laboratory. We also evaluated the shielding effectiveness of the experimental setup through an attenuation study. Our simulations indicate that the combined background from environmental gamma rays, neutrons, and muons in the relevant100Mo 0νββ Q-value region can be reduced to approximately 0.003 cts/kg/keV/yr.
