Tip
All input files can be downloaded: Files.
xpol
This option controls how to perform an XPol calculation.
Options
- method
Value
mndoam1am1drm1pm3pm3dpm6pmopmowDefault
am1Define semi-empirical quantum chemistry method used for XPol calculation:
- scf_type
Value
rfor restricted Hartree-Fockufor unrestricted Hartree-FockDefault
uDefine the SCF type for XPol calculation.
- non_var
Use non-variational XPol calculation.
- charge_type
Value
mullikenfor Mulliken chargesdppcfor DPPC chargesDefault
mullikenDefine the type of atomic charges used in XPol calculation.
- print_level
Value
PrintDetailsfor verbose output.PrintEssentialsfor standard output.PrintNonefor no output.Default
PrintEssentialsfor most cases.PrintNonechosen when running MD simulations.The information printing level.
- frag
This defines fragments divide for system. The format is:
frag autofor automatic fragmentation by connectivity, in which each fragment is assumed as 0 charge and spin multiplicity is 1.frag frag_charge frag_spin_multiplicity atom_rangeThere can be arbitrary number of fragments, but all atoms must be included once and only once.
Here is an example which defined two fragments, the first fragment has charge 0 and spin multiplicity 1, including atoms 1-3. And the second fragment has charge -1 and spin multiplicity 1, including atoms 4 and 5:
1xpol 2 frag 0 1 1-3 3 frag -1 1 4 5 4end
- lj
This defines Lennard-Jones parameters for non-bonded interactions between fragments. The format is:
lj element sigma(kcal/mol) epsilon(angstrom)Here is an example which defined Lennard-Jones parameters for oxygen:
xpol lj O 3.24 0.16 end
Lennard-Jones parameters DO HAVE a default value for each
method, which values will be shown in the output (withprint_levelbeingstandardorverbose).Users can set Lennard-Jones parameters to zero to turn off Lennard-Jones potential, but it is NOT recommended for most cases.
Theoretical Background
XPol (Explicit Polarization) method is an fragment-based molecular orbital method for macromolecular systems or as a quantum force field for biomolecular and materials simulations. In which the effective Hamiltonian of the system is defined as sum of the Hamiltonian of each fragment and the interaction between fragments:
where effective interaction \(H_ab\) is:
The first and second terms are the electrostatic interaction between fragment a and b. The third term is rest part of the interaction, including exchange-repulsion and dispersion, which is approximated by Lennard-Jones potential in Qbics. In Lennard-Jones potential:
where \(\sigma_{ij} = \sqrt{sigma_i sigma_j}\) and \(\epsilon_{ij} = \sqrt{\epsilon_i \epsilon_j}\)
Input Examples
Example: Geometry Optimization of a Water 32-mer Cluster
We perform an XPol(AM1) geometry optimization of a water 32-mer cluster. The input file is as follows:
1mol
2 O 97.87475883 102.91148275 100.43222418
3 H 98.10048536 102.79050385 99.49670462
4 H 96.95991242 102.56796734 100.50737622
5 O 101.67212251 100.66547197 98.58765134
6 H 102.52651498 100.96781895 98.89553074
7 H 101.15843794 100.69592086 99.38268162
8 O 102.52639867 102.62956434 93.30170631
9 H 103.16438994 102.36526190 93.95819868
10 H 102.63407183 102.01335071 92.58047987
11 O 99.78963345 100.83849646 101.54069420
12 H 99.30912663 100.01645853 101.39552030
13 H 99.23940855 101.52167838 101.13381944
14 O 96.56328196 97.88535664 96.50308776
15 H 97.35092126 98.00792877 97.04885973
16 H 96.69651386 98.57745337 95.81794455
17 O 101.55651965 100.44188235 104.28664047
18 H 101.29231198 100.93029165 103.49525059
19 H 100.94211385 99.69552549 104.31716088
20 O 98.33903077 98.20095050 100.62403173
21 H 97.46688986 98.39143429 100.24987990
22 H 98.88724929 98.01898905 99.85319955
23 O 96.49085505 98.39266949 102.98073892
24 H 97.01839676 97.82501901 102.38352998
25 H 97.07914726 99.11997116 103.16170500
26 O 100.15845368 103.89054070 94.76042836
27 H 100.31025871 104.78666572 94.46770421
28 H 100.85419073 103.40624744 94.34461276
29 O 103.25183143 96.43746872 100.41332692
30 H 103.57397677 95.82213950 101.06596184
31 H 103.15126935 97.25278259 100.91227387
32 O 97.13798587 100.54608198 95.60727695
33 H 97.64529580 101.01421113 96.29426155
34 H 97.34490899 101.02744763 94.81552265
35 O 102.78775615 103.10597939 102.69170404
36 H 101.87495620 103.36745217 102.55724327
37 H 103.06489064 103.57474280 103.47719197
38 O 105.53095101 101.29716070 98.21079885
39 H 105.03215048 101.37688198 99.04530056
40 H 106.25038600 100.74038966 98.47794141
41 O 98.70268843 95.52690714 102.59502954
42 H 99.17322933 95.31157551 101.76029157
43 H 97.90610766 95.03528662 102.53533381
44 O 103.78641524 101.15992809 95.54113067
45 H 104.39936744 101.10524187 96.28116776
46 H 102.97842339 100.71623589 95.82585034
47 O 95.22662726 101.25576753 100.54757706
48 H 95.09181455 100.34655632 100.81400025
49 H 94.38907591 101.45434975 100.11156173
50 O 95.54973945 98.46833715 99.41156281
51 H 94.70879499 98.48021487 99.90099164
52 H 95.30623251 98.85282300 98.57362839
53 O 100.12536081 98.01698448 103.79646915
54 H 99.68330998 97.64271317 103.01896562
55 H 100.30026427 97.24458856 104.34618200
56 O 106.60609274 101.92504242 101.89716471
57 H 106.84368696 102.84494573 102.05245773
58 H 105.66648449 101.93410939 101.68417941
59 O 100.01126957 103.86673296 102.85030571
60 H 99.14512402 103.81766227 102.41019067
61 H 99.80965676 103.94951879 103.78709147
62 O 93.81511560 98.54368963 101.94850824
63 H 93.22139837 98.39098127 102.70887412
64 H 94.70212504 98.47257445 102.33070353
65 O 99.08033419 102.19637632 96.96666652
66 H 99.38148657 102.93806620 96.41226668
67 H 99.89727554 101.78103607 97.26624567
68 O 101.36021466 95.92993105 98.33435488
69 H 100.79388068 95.36142415 98.89251709
70 H 102.12231924 96.11773498 98.89898325
71 O 94.18044332 99.98166565 97.13799412
72 H 93.84436158 100.73600892 96.58620048
73 H 94.62724720 99.39243988 96.51265012
74 O 98.94940687 94.18348363 99.84354786
75 H 98.20879957 94.58885710 99.34924055
76 H 99.10203464 93.34846140 99.38941413
77 O 103.67742801 101.36877267 100.57996535
78 H 103.42785492 102.04841830 101.23853223
79 H 103.65884497 100.55268424 101.08486536
80 O 96.65886667 95.34817030 98.48343811
81 H 96.53805782 95.50558559 97.54435890
82 H 96.21487869 96.11049225 98.89898081
83 O 106.02135041 99.68723306 103.72962852
84 H 106.52031039 100.10392218 103.02914526
85 H 106.17171080 100.23799272 104.50209644
86 O 103.99051333 101.25322961 105.92784042
87 H 103.63808059 100.87479551 106.74301354
88 H 103.38222106 100.95049676 105.22335194
89 O 103.18696851 98.59196287 102.47424149
90 H 102.38198604 98.93354192 102.90584555
91 H 103.86566109 98.70048906 103.16468216
92 O 99.62185304 98.43979440 97.89631983
93 H 100.20109427 99.22329848 97.85712762
94 H 100.18480479 97.73316108 97.59075637
95 O 100.50489514 103.29505799 106.03644982
96 H 100.84890641 102.48413426 105.65062052
97 H 100.94370169 103.40392719 106.88536708
98end
99
100xpol
101 scf_type u
102 charge_type dppc
103 frag auto
104end
105
106task
107 opt xpol
108end
You can change am1 to pm3, pm6, etc. to use other NDDO methods in XPol.
The optimization trajectory is shown below: