Net Transfer of “Negative Entropy”

Geology ◽  
2000 ◽  
Vol 28 (12) ◽  
pp. 1127-1130 ◽  
Author(s):  
Matthew J. Kohn ◽  
Frank Spear

1980 ◽  
Vol 16 (1) ◽  
pp. 103-109 ◽  
Author(s):  
L. Hertz ◽  
A. Yu ◽  
G. Svenneby ◽  
E. Kvamme ◽  
H. Fosmark ◽  
...  

1962 ◽  
Vol 203 (1) ◽  
pp. 73-80 ◽  
Author(s):  
James G. Manis ◽  
David Schachter

Everted gut sacs prepared from the proximal duodenum of the rat, mouse, and golden hamster can transfer iron actively, i.e. against concentration and potential gradients, from the mucosa to the serosa. The active transfer involves two steps: mucosal uptake and net transfer to the serosal surface. Oxidative metabolism is apparently required for each of the steps. Net transfer to the serosal surface is slower, more readily rate-limited, and more sharply localized to the proximal duodenum than is mucosal uptake. Both divalent and trivalent iron are taken up at the mucosal surface, but net transfer to the serosal surface is relatively specific for divalent iron. Calcium inhibits the net serosal transfer of iron at concentrations which do not inhibit the mucosal uptake. Parallel studies with loops of duodenum in living rats indicate that the active, two-step mechanism for iron absorption also functions in vivo, where the steps in the transfer are mucosal uptake followed by transport from the tissue to the blood stream.


2020 ◽  
Vol 112 (3) ◽  
pp. 576-585
Author(s):  
Katherine M Delaney ◽  
Ronnie Guillet ◽  
Eva K Pressman ◽  
Laura E Caulfield ◽  
Nelly Zavaleta ◽  
...  

ABSTRACT Background Maternal iron absorption during pregnancy can be evaluated using RBC incorporation of orally administered stable iron isotope. This approach underestimates true maternal absorption of iron as it does not account for absorbed iron that is transferred to the fetus or retained within the placenta. Objective Our objective was to re-evaluate maternal iron absorption after factoring in these losses and identify factors associated with iron partitioning between the maternal, neonatal, and placental compartments. Methods This study utilized data from stable iron isotope studies carried out in 68 women during the third trimester of pregnancy. Iron status indicators and stable iron isotopic enrichment were measured in maternal blood, umbilical cord blood, and placental tissue when available. Factors associated with iron isotope partitioning between the maternal, neonatal, and placental compartments were identified. Results On average, true maternal absorption of iron increased by 10% (from 19% to 21%) after accounting for absorbed iron present in the newborn (P < 0.001), and further increased by 7%, (from 39% to 42%, P < 0.001) after accounting for iron retained within the placenta. On average, 2% of recovered tracer was present in the placenta and 6% was found in the newborn. Net transfer of iron to the neonate was higher in women with lower total body iron (standardized β = −0.48, P < 0.01) and lower maternal hepcidin (standardized β = −0.66, P < 0.01). In women carrying multiple fetuses, neonatal hepcidin explained a significant amount of observed variance in net placental transfer of absorbed iron (R = 0.95, P = 0.03). Conclusions Maternal RBC iron incorporation of an orally ingested tracer underestimated true maternal iron absorption. The degree of underestimation was greatest in women with low body iron. Maternal hepcidin was inversely associated with maternal RBC iron utilization, whereas neonatal hepcidin explained variance in net transfer of iron to the neonatal compartment. These trials were registered at clinicaltrials.gov as NCT01019096 and NCT01582802.


1999 ◽  
Vol 303 (1-4) ◽  
pp. 193-222 ◽  
Author(s):  
Julie Newman ◽  
William M Lamb ◽  
Martyn R Drury ◽  
Reinoud L.M Vissers

Sign in / Sign up

Export Citation Format

Share Document