Supplementary Material (ESI) for Dalton Transactions This journal is (c) The Royal Society of Chemistry 2001 Table S3e. Anisotropic displacement parameters for Cu(glygly)(OH2)2.H2O at 10 K (XD) for XD multipole model. The anisotropic displacement factor exponent takes the form: -2.(pi)^2[h^2.a*^2.U11 + ... + 2.k.l.b*.c*.U23] Atom U11 U22 U33 U12 U13 U23 CuA 0.00361(4) 0.00557(4) 0.00398(4) -0.00009(3) 0.00092(2) 0.00040(3) O1A 0.0047(1) 0.0107(2) 0.0057(1) 0.0000(1) 0.0014(1) 0.0016(1) O2A 0.0047(1) 0.0123(2) 0.0062(1) 0.0002(1) 0.0002(1) 0.0018(1) O3A 0.0060(2) 0.0099(2) 0.0055(1) -0.0007(1) 0.0017(1) 0.0017(1) O4A 0.0060(1) 0.0090(2) 0.0075(1) 0.0000(1) 0.0021(1) 0.0020(1) O5A 0.0068(2) 0.0075(2) 0.0093(2) 0.0004(1) 0.0013(1) 0.0000(1) O6A 0.0094(2) 0.0091(2) 0.0086(2) 0.0015(1) 0.0030(1) 0.0015(1) N1A 0.0046(1) 0.0093(2) 0.0043(1) -0.0002(1) 0.0007(1) 0.0017(1) N2A 0.0054(1) 0.0091(2) 0.0065(1) -0.0009(1) 0.0008(1) 0.0008(1) C1A 0.0043(1) 0.0078(2) 0.0052(1) 0.0003(1) 0.0007(1) 0.0007(1) C2A 0.0049(1) 0.0085(2) 0.0053(1) -0.0004(1) 0.0012(1) 0.0008(1) C3A 0.0050(1) 0.0075(2) 0.0044(1) -0.0002(1) 0.0011(1) 0.0009(1) C4A 0.0057(2) 0.0103(2) 0.0058(1) -0.0004(1) 0.0002(1) 0.0016(1) CuB 0.00387(4) 0.00563(4) 0.00366(4) -0.00039(3) 0.00073(2) 0.00021(3) O1B 0.0057(1) 0.0102(2) 0.0047(1) -0.0019(1) 0.0010(1) 0.0003(1) O2B 0.0060(2) 0.0124(2) 0.0048(1) -0.0019(1) -0.0001(1) 0.0004(1) O3B 0.0063(2) 0.0111(2) 0.0067(2) -0.0025(1) 0.0024(1) -0.0007(1) O4B 0.0081(2) 0.0081(2) 0.0063(1) -0.0018(1) 0.0011(1) 0.0013(1) O5B 0.0100(2) 0.0085(2) 0.0079(2) 0.0015(1) 0.0026(1) 0.0006(1) O6B 0.0074(2) 0.0104(2) 0.0072(2) -0.0004(1) 0.0017(1) -0.0007(1) N1B 0.0046(1) 0.0091(2) 0.0045(1) -0.0011(1) 0.0006(1) 0.0002(1) N2B 0.0063(1) 0.0085(2) 0.0053(1) -0.0005(1) 0.0013(1) -0.0003(1) C1B 0.0050(1) 0.0079(2) 0.0045(1) -0.0005(1) 0.0007(1) 0.0002(1) C2B 0.0056(1) 0.0084(2) 0.0051(1) -0.0010(1) 0.0011(1) 0.0003(1) C3B 0.0045(1) 0.0077(2) 0.0055(1) -0.0007(1) 0.0013(1) -0.0004(1) C4B 0.0054(1) 0.0103(2) 0.0057(1) -0.0004(1) 0.0007(1) -0.0008(1)