“…Our positions of the Stark levels of the ground multiplet 2 F 7/2 , however, greatly differ. These positions were almost perfectly reproduced by our crystal field calculations knowing that the corresponding parameters were directly obtained from those derived in the case of Tm 3+ [6], by introducing between the respective parameters the multiplication factors a k such as B kq ðYb 3þ Þ ¼ a k B kq ðTm 3þ Þ and a k ¼ r k ðYb 3þ Þ=r k ðTm 3þ Þ ¼ 1.009, 0.9716, 0.9451 for k ¼ 2; 4; 6, respectively [7]. It was found B 20 ¼ 578 cm À1 , …”