From another vantage, departing from the classic organic chemistry depiction, I start with 2012 article in Atmospheric Chemistry and Physics 12, pages 6237–6271 (full paper ) regarding the haloform reaction in atmospheric conditions (and a path variation below for natural waters), to quote:
“Halocarbons can then be formed through the reaction of HOCl, HOBr and HOI with the dissolved organic matter through the haloform Reaction (R6, written for X = Cl), or less likely, through addition Reaction (R7).
RCOCH3 + 3 HOCl → RCOOH + CHCl3 + 2 H2O (R6) “
Based on the following comment on the reactivity of HOCl contained in this 2017 compilation by ScienceDirect at to quote:
“The reactivity of HO-Cl mimics those of the two-electron oxidation reaction exhibited by peroxynitrite (HO–NO2) or hydrogen peroxide (HO–OH) whereby the homolytic cleavage of O–X (X=N, O, or Cl) to form the HO and Cl pair could impart a diversity of chemical reactions with a variety of biomolecules.”
Based on the above and other mentioned radical pathways, I suggest the following largely radical pathway, letting G = RCO for convenience, assuming the presence of sunlight (or lab light) containing UV, as part of a hypochlorous acid activation path:
HOCl + hv → •OH + •Cl
Reference: See Scheme I and also a link to a free pdf download of the full paper, which I recommend, as this advanced work is replete with references to rRHS (radical Reactive Halogen Species) attacking organics.
Or, an alternate route per other sources including to quote “and HOCl can react in chloride containing aerosols to form Cl2. Cl2 can then escape to the gas phase and photolyze, releasing Cl atoms which may then reform HOCl” , and a similar observation in this full paper at, which also cites a role for natural organic matter (NOM) and HCO3- (contained also in some chlorine bleaches with added Na2CO3) acting as a catalyst.
Then, the proposed action of the hydroxyl radical (as frequently employed in environmental remediation, see as an example here ) together with the chlorine radical could continue as follows:
GCH3 + •OH + •Cl → •G + •CH2Cl + H2O
HOCl + hv → •OH + •Cl
•CH2Cl + •OH + •Cl → •CHCl2 + H2O
HOCl + hv → •OH + •Cl
•G + •OH → GOH
•CHCl2 + •Cl → CHCl3
Resulting in the cited net reaction for the haloform reaction in an assisted UV reaction (via possibly free liberated chlorine, NOM, HCO3-,..., per above references):
$$
GCH3 + 3 HOCl + hv → GOH + CHCl3 + 2 H2O
$$
Hypochlorous acid can also apparently be radicalized in the dark in the presence of transition metals occurring in natural waters in a Fenton-type reaction also per this reference:
$$
Fe(2+)/Cu(+) + HOCl → Fe(3+) + •ClOH-
$$
As such more generally, in the presence of a source of electrons (e.g. , Fe(2+) → Fe(3+) + e- ) and a medium that supports an electron’s half-life (like organics including humic acid and ethanol):
$$
HOCl + e- (aq) → •ClOH-
$$
With the created chlorine hydroxyl radical anion (above) displaying a pH dependence, with some authors assuming, contextually, an appropriate pH condition, citing different Fenton-type reaction products via hypochlorous, more explicitly:
At pH > 5 (Source: Scheme 1 reference above to quote: "Above pH >5 ketones and aldehydes are halogenated by electrophilic substitution at the α carbon"):
•ClOH- → •OH + Cl- (k = 6.1×10^9)
Source: See Reaction 6 at Supplement Table S1 at and click on Supplement pdf to download)
For completeness, at pH < 5:
$$
•ClOH- + H+ → H2O + •Cl (k = 21×10^9)
$$
Interestingly, the presence of chloride ion, can also be impactful, albeit slow, per the reaction:
$$
•ClOH- + Cl- → •Cl2- + OH- (k = 1.0 ×10^4)
$$
Where the dichloride radical anion (•Cl2-), while being less chemically reactive is, however, more stable and provides a source of •Cl (which slowing reacts with water liberating the hydroxyl radical at pH >5):
$$
•Cl + H2O → •ClOH- + H+ (k = 2.5×10^5)
$$
The Science Direct compilation also relatedly postulates a radical argument pathway with HOCl, to quote: “Reaction of HOCl with thiols yields RSOH via the radical–radical coupling reaction of the intermediates, RS• and HO•” displayed in Equations (2.77) to (2.79).