3 research outputs found
Backreaction in Axion Monodromy, 4-forms and the Swampland
Axion monodromy models can always be described in terms of an axion coupled
to 3-form gauge fields with non-canonical kinetic terms. The presence of the
saxions parametrising the kinetic metrics of the 3-form fields leads to
backreaction effects in the inflationary dynamics. We review the case in which
saxions backreact on the K\"ahler metric of the inflaton leading to a
logarithmic scaling of the proper field distance at large field. This behaviour
is universal in Type II string flux compactifications and consistent with a
refinement of the Swampland Conjecture. The critical point at which this
behaviour appears depends on the mass hierarchy between the inflaton and the
saxions. However, in tractable compactifications, such a hierarchy cannot be
realised without leaving the regime of validity of the effective theory,
disfavouring transplanckian excursions in string theory.Comment: Proceedings prepared for the "Workshop on Geometry and Physics",
November 2016, Ringberg Castl
Nitrogen Loss through Anaerobic Ammonium Oxidation Coupled to Iron Reduction from Paddy Soils in a Chronosequence
Anaerobic ammonium
oxidation coupled to ironÂ(III) reduction (termed
Feammox) with dinitrogen, nitrite, or nitrate as the end-product is
a recently discovered process of nitrogen cycling. However, Feammox
has not been described in paddy soils, which are rich in ironÂ(III)
oxides and subjected to intensive nitrogen fertilization. Here, evidence
for Feammox in a paddy soil chronosequence with a gradient of microbially
reducible ironÂ(III) levels was obtained in Southern China using <sup>15</sup>N-labeled ammonium-based isotopic tracing and acetylene inhibition
techniques. Our study demonstrated the occurrence of Feammox in the
chronosequence, and direct dinitrogen production was shown to be the
dominant Feammox pathway. Within the chronosequence, three paddy soils
with higher microbially reducible ironÂ(III) levels had higher Feammox
rates (ranged from 0.17 to 0.59 mg N kg<sup>–1</sup> d<sup>–1</sup>) compared to an uncultivated soil (0.04 mg N kg<sup>–1</sup> d<sup>–1</sup>). It is estimated that a loss
of 7.8–61 kg N ha<sup>–1</sup> year<sup>–1</sup> is associated with Feammox in the examined paddy soils. Overall,
we discover that rice cultivation could enrich microbially reducible
ironÂ(III), accelerate Feammox reaction and thus fuel nitrogen loss
from soils, and suggest that Feammox could be a potentially important
pathway for nitrogen loss in paddy soils
Application of Struvite Alters the Antibiotic Resistome in Soil, Rhizosphere, and Phyllosphere
Struvite recovered
from wastewater is a renewable source of phosphorus
and nitrogen and can be used as fertilizer for plant growth. However,
antibiotics and resistome can be enriched in the struvite derived
from wastewater. Robust understanding of the potential risks after
struvite application to soils has remained elusive. Here, we profiled
antibiotic resistance genes (ARGs) and mobile genetic elements (MGEs)
in struvite, soil, rhizosphere and phyllosphere of <i>Brassica</i> using high-throughput quantitative PCR. A total of 165 ARGs and
10 MGEs were detected. Application of struvite was found to increase
both the abundance and diversity of ARGs in soil, rhizosphere and
phyllosphere. In addition, ARGs shared exclusively between <i>Brassica</i> phyllosphere and struvite were identified, indicating
that struvite was an important source of ARGs found in phyllosphere.
Furthermore, OTUs shared between rhizosphere and phyllosphere were
found to significantly correlate with ARGs, suggesting that microbiota
in leaf and root could interconnect and ARGs might transfer from struvite
to the surface of plants via rhizosphere using bacteria as spreading
medium. These findings demonstrated that struvite as an organic fertilizer
can facilitate the spread of antibiotic resistance into human food
chain and this environment-acquired antibiotic resistance should be
put into human health risk assessment system