minerals
Article
Fractions of Ni, Pb, Cr, and Their Impact on Enzyme Activities
of Arable Land Cultivated by the Simplified Method
Adam Lukowski
1,
* and Dorota Dec
2
Citation: Lukowski, A.; Dec, D.
Fractions of Ni, Pb, Cr, and Their
Impact on Enzyme Activities of
Arable Land Cultivated by the
Simplified Method. Minerals 2021, 11,
584. https://doi.org/10.3390/
min11060584
Academic Editor:
Maria Economou-Eliopoulos
Received: 20 April 2021
Accepted: 28 May 2021
Published: 31 May 2021
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1
Department of Technology in Environmental Engineering, Institute of Environmental Engineering and
Energy Production, Faculty of Civil Engineering and Environmental Sciences, Bialystok University of
Technology, Wiejska 45A, 15-351 Bialystok, Poland
2
Department of Agri-Food Engineering and Environmental Management, Institute of Environmental
Engineering and Energy Production, Faculty of Civil Engineering and Environmental Sciences, Bialystok
University of Technology, Wiejska 45A, 15-351 Bialystok, Poland; d.dec@pb.edu.pl
* Correspondence: a.lukowski@pb.edu.pl
Abstract: Total metal content is not representing its availability and thus does not provide the
details about potential environmental hazards, including the impact on soil enzyme activities. To
understand metal availability, chemical fractions must be considered. The goal of this study was
to evaluate the influence of Ni, Cr, and Pb fractions on the enzymatic activity of soils cultivated
by the simplified method, which is rare not only in Poland. The percentage of studied metals in
fractions was determined according to the Community Bureau of Reference (BCR) method. Four
fractions were extracted: acid soluble and exchangeable (F1), reducible (F2), oxidizable (F3), and
residual (F4). The highest Ni and Cr percentages were noted in fraction F4, and for Pb, they were
noted in fraction F2. The smallest Ni and Pb percentages were observed in fraction F1 (most mobile)
and for Cr, they were observed in fraction F2. In soil samples collected in spring, the significant
relationship was stated between F1/Ni/dehydrogenase, F2/Pb/dehydrogenase, and F2/Pb/urease.
Such dependence occurred between F1/Ni/phosphatase and F4/Ni/urease during summer as well
as between F1/Ni/phosphatase and F4/Ni/dehydrogenase in autumn. F1/Pb caused a drop in
phosphatase activity, whereas F4/Cr influenced its increase. The study results indicated that metal
fractions influenced phosphatase activity the most, while protease activity in the soil was not affected.
Keywords: metal fraction; enzyme activity; heavy metal; arable soil; BCR method
1. Introduction
Soil is a very important part of the ecosystem. Heavy metals in soil represent de-
structive and potent environmental hazards [1]. They are a source of concern because
of their potential reactivity, toxicity, and mobility [2,3]. High concentrations of metals in
soil can cause the limitation of vegetation [4]. According to Xia et al. [5], nickel toxicity
toward microorganisms in soil appears at concentrations higher than 100 mg kg
−1
, causing
the decrease of microbial biomass carbon and soil basal respiration. As to lead, the toxic
level is 150 mg kg
−1
for microbial biomass carbon and 100 mg kg
−1
for microbial biomass
nitrogen [6]. Chromium belongs to the metals that are extremely harmful to microbes. In
the environment, only trivalent and hexavalent forms of chromium are prevalent. They are
differentiated in terms of biological reactivity and physicochemical properties. Hexavalent
ions are more toxic due to the high mobility in biological systems [7]. As stated by ul
Hassan et al. [8], the 50% reduction in overall microbial soil activity is observed at a total
chromium concentration of 263 g kg
−1
. The toxicity of heavy metals to plants is dependent
on soil composition, plant species, metal concentration, soil pH, and the chemical form of
the metal [9]. Critical concentrations in soil are within the range of 10–100, 30–300, and
5–30 mg·kg
−1
for Ni, Pb, and Cr, respectively [10]. The persistence of enzymes in the soil
is influenced by parameters such as soil temperature, depth, organic matter, acidity, and
Minerals 2021, 11, 584. https://doi.org/10.3390/min11060584 https://www.mdpi.com/journal/minerals