66 research outputs found
Seasonal variations of soil microbial biomass carbon (C) and nitrogen (N), soil microbial activity and microbial metabolic quotient (<i>q</i>CO<sub>2</sub>) in the 0 - 10 cm soil layer as influenced by carbon addition (+60%) and water addition (+30%) in temperate steppe of northeastern China.
<p>Values show the monthly means from June to September in the two growing seasons. Vertical bars indicate standard errors of means (n = 6). Difference lowercase letters indicate statistically significant differences (<i>P</i><0.05). A = ambient condition (control), C = carbon addition, W = water addition, CW = combined carbon and water additions.</p
Responses of soil organic carbon (C), total nitrogen (N) and inorganic N content to carbon addition (+60%) and water addition (+30%) during the two growing seasons in temperate steppe of northeastern China.
<p>Vertical bars indicate standard errors of means (n = 6). Difference lowercase letters indicate statistically significant differences (<i>P</i><0.05). A = ambient condition (control), C = carbon addition, W = water addition, CW = combined carbon and water additions.</p
Results (<i>F</i>-values) of Three-way ANOVAs on the effects of carbon addition (C), water addition (W), year (Y), and their interactions on soil organic C (SOC), soil total N (TN), aboveground biomass C (ABC) and N (ABN), root biomass C (RBC) and N (RBN), grass biomass (GB), forb biomass (FB) and the ratio of grass to forb biomass (GB: FB).
*<p>
<i>represents significant at P<0.05.</i></p
Figure 1
<p>Daily precipitation (bars) and daily mean air temperature (line) in 2010 and 2011 (A). Data are from the eddy tower adjacent (approximately 100 m) to the experimental site. Seasonal variations of soil temperature (B) and water content (C) at topsoil layer (0–10 cm) in response to carbon addition (+60%) and water addition (+30%) in the temperate steppe of northeastern China. Insets represent the two seasonal mean values of soil temperature (ST) and water content (SWC). Vertical bars indicate standard errors of means (n = 6). Difference lowercase letters indicate statistically significant differences (<i>P</i><0.05). A = ambient condition (control), C = carbon addition, W = water addition, CW = combined carbon and water additions.</p
Responses of aboveground biomass carbon (C) and nitrogen (N), root biomass C and N, peak aboveground biomass of grass and forb and the grass: forb ratio to carbon addition (+60%) and water addition (+30%) in 2010 and 2011 in temperate steppe of northeastern China.
<p>Vertical bars indicate standard errors of means (n = 6). Difference lowercase letters indicate statistically significant differences (<i>P</i><0.05). A = ambient condition (control), C = carbon addition, W = water addition, CW = combined carbon and water additions.</p
Results (<i>F</i>-values) of Four-way ANOVAs on the effects of carbon addition (C), water addition (W), sampling date (D), year (Y), and their interactions on soil temperature (ST), soil water content (SWC), microbial biomass C (MBC), microbial biomass N (MBN), microbial activity (SMA), metabolic quotient (<i>q</i>CO<sub>2</sub>), soil inorganic N (IN), soil total PLFAs (TP), contribution of soil fungal PLFAs (F) and bacterial PLFAs (B), and the ratio of fungal to bacterial PLFAs (F: B).
*<p>, **, <i>and</i> ***<i>represent significant at P<0.05, 0.01, and 0.001, respectively.</i></p
The total biomass phospholipid fatty acids (PLFAs), percentages of fungal and bacterial PLFAs to the total biomass PLFAs, and the ratio of fungal to bacterial PLFAs as influenced by carbon addition (+60%) and water addition (+30%) in temperate steppe of northeastern China.
<p>Values show the monthly means from June to September in the growing season. Vertical bars indicate standard errors of means (n = 6). Difference lowercase letters indicate statistically significant differences (<i>P</i><0.05). A = ambient condition (control), C = carbon addition, W = water addition, CW = combined carbon and water additions.</p
Influence of Water on Protein Transitions: Morphology and Secondary Structure
Fibrous protein secondary structural
transitions are affected by
bound water. A family of specially designed recombinant spider silk-like
block copolymers with a gradient of block length, hydrophobilicity,
and degree of crystallinity was biosynthesized and characterized to
demonstrate the effect of water on the protein structural transitions.
These proteins were inspired by the genetic sequences found in the
dragline silk of <i>Nephila clavipes</i>, comprising an
alanine-rich hydrophobic block, A, a glycine-rich hydrophilic block,
B, and a C-terminus or a His-tag, H. Because the A-block is hydrophobic
and the B-block is hydrophilic, the spider silk-like block copolymers
behave as amphiphilic molecules and self-assemble into various structures
in water solution. We employ time-resolved Fourier transform infrared
(FTIR) spectroscopy to assign the origin of specific secondary structural
transitions during heating. A transition from random coils to β-turns
dominates during a lower temperature glass transition (of plasticized
protein) mediated by the removal of bound water. Once the protein
is in the dry solid state, further heating causes the now-dry protein
to undergo the glass transition to the liquid state through conversion
of α-helices into β-turns. The structural transitions
during protein glass transitions are intrinsic to the amorphous region
of protein and are hardly affected by protein hydrophobicity, block
length, or crystallinity. The self-assembly morphology of the spider
silk-like block copolymers, investigated by scanning electron microscopy,
indicates that the large-scale morphology is stable during heating
through both the lower and upper temperature glass transitions
Modeling and Experiment Reveal Structure and Nanomechanics across the Inverse Temperature Transition in <i>B. mori</i> Silk-Elastin-like Protein Polymers
Silk
and elastin are exemplary protein materials that exhibit exceptional
material properties. Silk is uniquely strong, surpassing engineering
materials such as Kevlar and steel, while elastin has exquisite flexibility
and can reversibly fold into a more structured form at high temperatures
when many other proteins would unfold and denature. This phenomenon
in elastin is termed the inverse temperature transition. It is a reversible,
controllable process that motivates applications in drug delivery,
shape change materials, and biomimetic devices. Silk-elastinlike protein
polymers (SELPs), which combine repeating <i>B. mori</i> silk and elastin blocks, have been introduced as biologically inspired
materials that combine the distinctive properties of the component
parts to achieve strong and extensible, tunable biomaterials. Here,
we considered a single SELP sequence to examine temperature transition
effects at the molecular scale. SELP molecular models were created
using Replica Exchange Molecular Dynamics, an accelerated sampling
method, and confirmed in experiment by comparing secondary structure
distributions. A molecular collapse of the SELP molecule was observed
with increased temperature in both molecular simulation and experiment.
Temperature-specific differences were observed in the mechanical properties
and the unfolding pathways of the polypeptide. Using the Bell–Evans
model, we analyzed the free energy landscape associated with molecular
unfolding at temperatures below and above the transition temperature
range (<i>T</i><sub>t</sub>) of the polypeptide. We found
that at physiological pulling rates, the energy barrier to unfold
SELPs was counterintuitively higher above <i>T</i><sub>t</sub>. Our findings offer a foundational perspective on the molecular
scale mechanisms of temperature-induced phase transition in SELPs,
and suggest a novel approach to combine simulation and experiment
to study materials for multifunctional biomimetic applications
Single-Nucleobase-Resolved Nanoruler Determines the Surface Energy Transfer Radius on the Living Cell Membrane
Investigations about surface energy transfer radius (r0) are limited to the aqueous solution system,
and it
is quite limited on experimental values of r0 between dyes and the corresponding gold particle (AuNP) sizes,
especially for living cell systems. Hence, the selection of suitable
AuNP-dye pairs is restricted when designing nanometal surface energy
transfer (NSET) strategies in analytical sciences. Here, we developed
a single-nucleobase-resolved NSET strategy to in situ measure the r0 value between a specific
dye and different-sized AuNPs on the living cell membrane. Using the
aptamer-dye complex (XQ-2d-nTA-FAM) and antiCD71
antibody-coupled AuNP conjugate (Au@antiCD71) as two working elements
to bind two different sites on CD71 receptors on living cell membranes,
we modified the nTA spacer between FAM and the terminal
of aptamer to change the distance (r) from FAM to
AuNP center and further adjusted the quenching efficiency (Φ)
between them. Different r0 values of various
AuNP-FAM pairs in living cells are determined by this in situ detection strategy. Based on this single-nucleobase-resolved NSET
strategy, we established a simple and efficient universal method for
measuring r0 in the living cell system,
which greatly expanded the selection range of AuNP-dye pairs during
the construction of the NSET model at the nanoscale
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