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@ARTICLE{Mohseni:902961,
author = {Mohseni, Neda and Bol, Roland},
title = {{V}ariation in the rate of land subsidence induced by
groundwater extraction and its effect on the response
pattern of soil microbial communities},
journal = {Earth surface processes and landforms},
volume = {46},
number = {10},
issn = {0197-9337},
address = {New York, NY [u.a.]},
publisher = {Wiley},
reportid = {FZJ-2021-04707},
pages = {1898 - 1908},
year = {2021},
abstract = {Excessive extraction of groundwater leads to (irreversible)
changes in the physical soil properties, causing land
subsidence associated with soil compaction to occur. Using a
combined image processing and field approach, we examined:
(1) how variation in the land subsidence rate induces
different soil compaction degrees; and (2) the response
patterns of microbial communities to such variations. By
using Sentinel Synthetic Aperture Radar image processing, we
selected three locations that exhibited different land
subsidence rates, including high (HSR), moderate (MSR), and
low (LSR). Then, soil sampling was undertaken within these
representative locations. Indicators of soil compaction,
including total porosity, air-filled porosity, water-filled
porosity, and bulk density, were measured. The soil
microbial community was determined using qPCR and
sequencing. The highest and lowest values for bulk density
were observed in the HSR–MSR and LSR zones, respectively.
The greatest values of total porosity and macropore volume
were displayed in the LSR zone compared to other zones.
Bacterial abundance in the LSR zone was significantly
greater than that in the HSR and MSR zones. The relative
abundances of bacterial taxa indirectly demonstrated that
the anaerobic phyla were significantly increased (by
$10–13\%),$ and the aerobic phyla decreased (by
$30–40\%)$ in the HSR zone compared to the LSR zone. This
result demonstrates that the aerobes declined as larger
volumes of the soil became more anaerobic. Indeed, the
increased abundance of anaerobes was not able to compensate
for the larger decrease in the abundance of aerobes. Our
work showed that at the increased rates of land subsidence,
the abundance distribution of the microbial community
critically declined. These findings highlight the critical
impacts of increasing the land subsidence rate on the
emergence of high soil compaction degrees, which can
significantly affect the resilience thresholds of the
microbial communities in dryland soils.},
cin = {IBG-3},
ddc = {910},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217)},
pid = {G:(DE-HGF)POF4-2173},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000652823200001},
doi = {10.1002/esp.5133},
url = {https://juser.fz-juelich.de/record/902961},
}