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Summary Background Anti‐tumour necrosis factor (TNF) agents are effective in Crohn's disease but some patients lose response and require alternative biologic therapy. There are few data on comparative effectiveness of vedolizumab and ustekinumab in this setting. Aim To compare the effectiveness of ustekinumab and vedolizumab in anti‐TNF‐refractory Crohn's disease over 12 months. Methods Patients commencing ustekinumab or vedolizumab for anti‐TNF‐refractory Crohn's disease with minimum follow‐up of 12 months were included. The primary outcome measure was the difference in steroid‐free remission rates at end of induction (2 months) and at 12 months. We also assessed rates of clinical response and remission, treatment persistence, surgery and adverse events in both groups. We performed logistic regression analysis to assess factors associated with steroid‐free remission and clinical response and remission. Results We included 85 patients commencing vedolizumab and 45 commencing ustekinumab. In an unadjusted model, rates of steroid‐free and clinical remission were significantly higher among ustekinumab‐treated patients. After adjusting for confounders, steroid‐free remission was higher among ustekinumab‐treated patients at 2 months (odds ratio, OR 2.79, 95% confidence interval, CI 1.06‐7.39, P = 0.038) and 12 months (OR 2.01, 95% CI 0.89‐4.56, P = 0.095). More patients treated with ustekinumab remained on therapy at the end of 12 months (84.4% vs 61.5%, P = 0.007). Conclusions Ustekinumab appeared more effective in treating anti‐TNF‐refractory Crohn's disease and more patients persisted with therapy.

Amorphous ices govern a range of cosmological processes and are potentially key materials for explaining the anomalies of liquid water. A substantial density gap between low-density and high-density amorphous ice with liquid water in the middle is a cornerstone of our current understanding of water. However, we show that ball milling “ordinary” ice I h at low temperature gives a structurally distinct medium-density amorphous ice (MDA) within this density gap. These results raise the possibility that MDA is the true glassy state of liquid water or alternatively a heavily sheared crystalline state. Notably, the compression of MDA at low temperature leads to a sharp increase of its recrystallization enthalpy, highlighting that H 2 O can be a high-energy geophysical material.