Examination of residual chloroform interference in the measurement
of microbial biomass C by fumigation-extraction
Nativ Rotbart
a, b
, Mikhail Borisover
a
, Nadezhda Bukhanovsky
a
, Alla Nasonova
a
,
Asher Bar-Tal
a
, Adi Oren
a, *
a
Department of Soil Chemistry, Plant Nutrition and Microbiology, Institute of Soil, Waterand Environmental Sciences, Volcani Center, Agricultural Research
Organization (ARO), Rishon LeZion 75359, Israel
b
Department of Soil and Water Sciences, Faculty of Agriculture, Environment and Food Sciences, The Hebrew University of Jerusalem, Rehovot, Israel
article info
Article history:
Received 13 January 2017
Received in revised form
5 March 2017
Accepted 29 March 2017
Keywords:
Chloroform fumigation-extraction
Residual chloroform
Soil moisture level
Procedure validity
Soil microbial biomass
abstract
Using the chloroform fumigation-extraction (CFE) method for determining microbial biomass in soils, a
presumption is followed, i.e., that chloroform becomes fully evacuated from the fumigated soil before
extraction. Otherwise, the C-containing fumigant may comprise an unknown part of the extractable C
flush, resulting in certain overestimation of soil microbial biomass. A quantitative assessment of
extractable residual chloroform levels in fumigated soils was performed, testing soils varying in clay and
organic matter contents. The tests were performed over a broad range of soil moisture conditions as to
facilitate a mechanistic interpretation of possible chloroform interactions in the studied soils (i.e.,
dissolution, sorption). The results support the validity of the CFE method's application in agricultural
soils, demonstrating the insignificance of biomass overestimation arising from residual chloroform.
© 2017 Published by Elsevier Ltd.
1. Introduction
Chloroform fumigation-extraction (CFE) is by far the most
widely used method for determining microbial biomass in soils.
The pioneering work of Vance et al. (1987) has been cited 6899
times, third of the citing papers being published since 2013 (Google
Scholar; accessed at March 5, 2017). The attractiveness of the
method arises from the ability to assess the bulk microbial biomass
C (or N) rather than just biomarker compounds such as ATP,
phospholipids or nucleic acids (Blagodatskaya and Kuzyakov, 2013).
Using the CFE method, a presumption is followed, i.e., that chlo-
roform becomes fully evacuated from the fumigated soil before
extraction. Otherwise, the C-containing fumigant may comprise an
unknown part of the extractable C flush, resulting in certain over-
estimation of soil microbial biomass. Yet, to the best of our
knowledge, evidence for complete evacuation of the chloroform
has never been presented. Moreover, the use of smell as means of
residual chloroform detection has been explicitly reported in the
publication formally prescribing the chloroform fumigation-
incubation method preceding the CFE method (Jenkinson and
Powlson, 1976) as well as in the Laboratory Manual of the Soil
Microbial Biomass Group at the Rothamsted Experimental Station
(Grace et al., 2006). It should be emphasized that solubility of
chloroform in water is not negligible (8416 mg l
1
at 21
C; Chen
et al., 2012). Hence, fumigation of soil maintained at 40% water
holding capacity (WHC) as prescribed by Vance et al. (1987) or at
50e60% WHC as found by Ross (1989) to yield maximum
extractable-C flush values, might result in certain levels of chloro-
form dissolution in soil water as governed by Henry's law (Ong and
Lion, 1991). Alternatively, chloroform vapor may undergo sorption
interactions with soil clay and/or organic matter (SOM) constitu-
ents (Chen and Dural, 2002), possibly hindering its evacuation as
well. To our knowledge, only a single work by Alessi et al. (2011)
contended with the risk of residual chloroform in the CFE proced-
ure, alarmingly reporting significant chloroform levels remaining in
the extracts from two fumigated natural loam soils, as well as from
pure clay minerals-particularly in their hydrated state. Attempts to
remove the chloroform prior to extraction by increasing the evac-
uation time, or to remove chloroform in the extracts by sparging
them vigorously with nitrogen gas, both failed.
The main goal of the current study was to quantify extractable
residual chloroform levels in fumigated soils, testing soils varying
* Corresponding author.
E-mail address: adior@volcani.agri.gov.il (A. Oren).
Contents lists available at ScienceDirect
Soil Biology & Biochemistry
journal homepage: www.elsevier.com/locate/soilbio
http://dx.doi.org/10.1016/j.soilbio.2017.03.018
0038-0717/© 2017 Published by Elsevier Ltd.
Soil Biology & Biochemistry 111 (2017) 60e65