A new frustrated triangular lattice antiferromagnet Na_(2)BaNi(PO_(4))_(2) was synthesized by high temperature flux method.The two-dimensional triangular lattice is formed by the Ni^(2+)ions with S=1.Its magnetism is ...A new frustrated triangular lattice antiferromagnet Na_(2)BaNi(PO_(4))_(2) was synthesized by high temperature flux method.The two-dimensional triangular lattice is formed by the Ni^(2+)ions with S=1.Its magnetism is highly anisotropic with the Weiss constants θCW=6.615 K(H||c)and43.979 K(H⊥c).However,no magnetic ordering is present down to 0.3 K,reflecting strong geometric spin frustration.Our heat capacity measurements show substantial residual magnetic entropy existing below 0.3 K at zero field,implying the presence of low energy spin excitations.These results indicate that Na_(2)BaNi(PO_(4))_(2) is a potential spin liquid candidate with spin-1.展开更多
Land-sea breeze(LSB)is an atmospheric mesoscale circulation that occurs in the vicinity of the coast and is caused by uneven heating resulting from the difference in specific heat capacity between the sea and land sur...Land-sea breeze(LSB)is an atmospheric mesoscale circulation that occurs in the vicinity of the coast and is caused by uneven heating resulting from the difference in specific heat capacity between the sea and land surfaces.The circulation structure of LSB was quantitatively investigated with a Doppler wind lidar Windcube100s on the west coast of the Yellow Sea for the first time.The time of observation was 31 August to 28 September 2018.It was found that the height of LSB development was 700 m to 1300 m.The duration of conversion of LSB was between 6 h and 8 h.The biggest average horizontal sea-breeze wind speed at 425 m was 5.6 m s^(-1),and at 375 m it was 4.5 m s^(-1).During the conversion process from sea breeze to land breeze,the maximum wind shear exponent was 2.84 at 1300 m altitude.During the conversion process from land breeze to sea breeze,the maximum wind shear exponent was 1.28 at 700 m altitude.The differences in wind shear exponents between sea-breeze and landbreeze systems were between 0.2 and 3.6 at the same altitude.The maximum value of the wind shear exponent can reflect the height of LSB development.展开更多
基金Project supported by the National Natural Science Foundation of China(Grant No.11804137)the Natural Science Foundation of Shandong Province,China(Grant Nos.ZR2020YQ03 and ZR2018BA026).
文摘A new frustrated triangular lattice antiferromagnet Na_(2)BaNi(PO_(4))_(2) was synthesized by high temperature flux method.The two-dimensional triangular lattice is formed by the Ni^(2+)ions with S=1.Its magnetism is highly anisotropic with the Weiss constants θCW=6.615 K(H||c)and43.979 K(H⊥c).However,no magnetic ordering is present down to 0.3 K,reflecting strong geometric spin frustration.Our heat capacity measurements show substantial residual magnetic entropy existing below 0.3 K at zero field,implying the presence of low energy spin excitations.These results indicate that Na_(2)BaNi(PO_(4))_(2) is a potential spin liquid candidate with spin-1.
基金supported by the National Key Research and Development Program of China[Grant number 2016YFC0202001]the Chinese Academy of Sciences Strategic Priority Research Program[Grant number XDA23020301]the National Natural Science Foundation of China[Grant number 41375036]。
文摘Land-sea breeze(LSB)is an atmospheric mesoscale circulation that occurs in the vicinity of the coast and is caused by uneven heating resulting from the difference in specific heat capacity between the sea and land surfaces.The circulation structure of LSB was quantitatively investigated with a Doppler wind lidar Windcube100s on the west coast of the Yellow Sea for the first time.The time of observation was 31 August to 28 September 2018.It was found that the height of LSB development was 700 m to 1300 m.The duration of conversion of LSB was between 6 h and 8 h.The biggest average horizontal sea-breeze wind speed at 425 m was 5.6 m s^(-1),and at 375 m it was 4.5 m s^(-1).During the conversion process from sea breeze to land breeze,the maximum wind shear exponent was 2.84 at 1300 m altitude.During the conversion process from land breeze to sea breeze,the maximum wind shear exponent was 1.28 at 700 m altitude.The differences in wind shear exponents between sea-breeze and landbreeze systems were between 0.2 and 3.6 at the same altitude.The maximum value of the wind shear exponent can reflect the height of LSB development.
