Stream water age distributions controlled by storage dynamics and nonlinear hydrologic connectivity : Modeling with high-resolution isotope data

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Using geophysical surveys to test tracer-based storage estimates in headwater catchments

Acknowledgements The authors are grateful to Stian Bradford, Chris Gabrielli, and Julie Timms for practical and logistical assistance. The provision of transport by Iain Malcolm and Ross Glover of Marine Scotland Science was greatly appreciated. We also thank the European Research Council ERC (project GA 335910 VEWA) for funding through the VeWa project and the Leverhulme Trust for funding through PLATO (RPG-2014-016).Peer reviewedPostprin

Procedure-related risk of miscarriage following chorionic villus sampling and amniocentesis

Objective: The objective of our study was to estimate the procedure-related risks of miscarriage following CVS and amniocentesis in a large unselected screened and to determine whether these risks are consistent with those reported in systematic reviews and meta-analysis. Methods: This was a retrospective cohort study undertaken at a large Fetal Medicine Unit in the United Kingdom during the period of January 2009 to May 2018. We included all singleton pregnancies that booked at our unit before 20 weeks after excluding those with multiple pregnancies, major fetal defects, terminations and lost to follow-up. We estimated the risk of miscarriage in those that had a CVS or amniocentesis as well as those that did not have any invasive procedure, to estimate the procedure-related risk as a risk-difference (95% confidence interval [CI]). Univariate and multivariate regression analysis was used to derive odds ratios (OR) (95%CI) and determine which maternal and pregnancy characteristics provided a significant contribution in prediction of miscarriage and whether CVS or amniocentesis provided a significant independent. Results: During the study period, there were 45,120 singleton pregnancies, including 1,546 that had an invasive procedure. We excluded 1,429 pregnancies (3.2%), due to fetal defects, termination of pregnancy or those with missing outcomes. In pregnancies that underwent CVS, the risk of miscarriage was 1.5% (13/861), compared to 1.2% (476/39,152) in pregnancies that did not have a procedure (p=0.437). In pregnancies that underwent an amniocentesis, the risk of miscarriage was 0.8% (3/375), compared to 1.2% (491/42,463) in those that did not (p=0.520). Univariate and multivariate regression analysis demonstrated that there was no significant prediction to the risk of miscarriage from CVS (p=0.399; p=0.592, respectively) or amniocentesis (p=0.543; p=0.550, respectively). The risk of procedure-related loss attributed to CVS was 0.29% (95%CI: -0.53-1.12) and that following amniocentesis was -0.36% (95%CI: -1.26-0.55), which was not significantly different from those that did not have any procedure. Conclusion: The procedure-related risks of miscarriage following CVS and amniocentesis are considerably lower than currently quoted. The estimates of risks based on our study are 0.29% for CVS and -0.36 for amniocentesis

Prevention of stillbirths: impact of a two-stage screening for vasa previa

Objectives: To examine the feasibility and effectiveness of a two-stage ultrasound screening strategy for detection of vasa previa and estimate the potential impact of screening on prevention of stillbirth. Methods: This was a retrospective examination of data from prospective screening for vasa previa in singleton pregnancies undertaken at the Fetal Medicine Centre at Medway Maritime Hospital, UK between 2012 and 2018. Women booked for prenatal care and delivery in our hospital had routine ultrasound examinations at 11-13 and 20-22 weeks’ gestation. Those with velamentous cord insertion at the inferior part of the placenta at the first-trimester scan and those with low-lying placenta at the second-trimester scan were classified as high-risk for vasa previa and had transvaginal sonography specifically searching for vasa previa at the time of the 20-22 weeks scan. The management and outcome of cases with suspected vasa previa is described. We excluded cases of miscarriage or termination at <24 weeks’ gestation. Results: The study population of 26,830 singleton pregnancies, included 21 (0.08% or 1 in 1,278) with vasa previa. In all cases of vasa previa the diagnosis was made at the 20-22 weeks scan and confirmed by gross and histological examination of the placenta postnatally. At the 11-13 weeks scan the cord insertion was classified as central in 25,071 (93.4%) cases, marginal in 1,680 (6.3%), and velamentous in 79 (0.3%). In 16 (76.2%) of the 21 cases of vasa previa, the cord insertion at the first-trimester scan was classified as velamentous at the inferior part of the placenta, in 2 (9.5%) as marginal and in 3 (14.3%) as central. The 21 cases of vasa previa were managed on an outpatient basis with serial scans for measurement of cervical length and elective cesarean section at 34 weeks’ gestation; all babies were liveborn but there was one neonatal death. In the study population there were 83 stillbirths and postnatal examination showed no evidence of vasa previa in any of the cases. On the assumption that if we had not diagnosed prenatally all 21 cases of vasa previa in our population half of these cases would have resulted in stillbirth, then the potential impact of screening is prevention of 9.6% (10/104) of stillbirths. Conclusion: A two-stage strategy of screening for vasa previa can be incorporated into routine clinical practice and such strategy could potentially reduce the rate of stillbirth

Using geophysical surveys to test tracer-based storage estimates in headwater catchments

Hydrogeophysical surveys were carried out in a 3.2 km2 Scottish catchment where previous isotope studies inferred significant groundwater storage that makes important contributions to streamflow. We used electrical resistivity tomography (ERT) to characterize the architecture of glacial drifts and make an approximation of catchment‐scale storage. Four ERT lines (360–535 m in length) revealed extensive 5–10 m deep drift cover on steeper slopes, which extends up to 20–40 m in valley bottom areas. Assuming low clay fractions, we interpret variable resistivity as correlating with variations in porosity and water content. Using Archie's Law as a first approximation, we compute likely bounds for storage along the ERT transects. Areas of highest groundwater storage occur in valley bottom peat soils (up to 4 m deep) and underlying drift where up to 10 000 mm of precipitation equivalent may be stored. This is consistent with groundwater levels which indicate saturation to within 0.2 m of the surface. However, significant slow groundwater flow paths occur in the shallower drifts on steeper hillslopes, where point storage varies between ~1000 mm–5000 mm. These fluxes maintain saturated conditions in the valley bottom and are recharged from drift‐free areas on the catchment interfluves. The surveys indicate that catchment scale storage is >2000 mm which is consistent with tracer‐based estimates. Copyright © 2016 John Wiley & Sons, Ltd

Depth distribution of soil water sourced by plants at the global scale : a new direct inference approach

Funding Information Fondazione Cassa di Risparmio di Padova e Rovigo. Grant Number: Bando Starting Grants 2015Peer reviewedPostprin

Occurrence and Treatment of Bone Atrophic Non-Unions Investigated by an Integrative Approach

Recently developed atrophic non-union models are a good representation of the clinical situation in which many nonunions develop. Based on previous experimental studies with these atrophic non-union models, it was hypothesized that in order to obtain successful fracture healing, blood vessels, growth factors, and (proliferative) precursor cells all need to be present in the callus at the same time. This study uses a combined in vivo-in silico approach to investigate these different aspects (vasculature, growth factors, cell proliferation). The mathematical model, initially developed for the study of normal fracture healing, is able to capture essential aspects of the in vivo atrophic non-union model despite a number of deviations that are mainly due to simplifications in the in silico model. The mathematical model is subsequently used to test possible treatment strategies for atrophic non-unions (i.e. cell transplant at post-osteotomy, week 3). Preliminary in vivo experiments corroborate the numerical predictions. Finally, the mathematical model is applied to explain experimental observations and identify potentially crucial steps in the treatments and can thereby be used to optimize experimental and clinical studies in this area. This study demonstrates the potential of the combined in silico-in vivo approach and its clinical implications for the early treatment of patients with problematic fractures

Advancing osteochondral tissue engineering: bone morphogenetic protein, transforming growth factor, and fibroblast growth factor signaling drive ordered differentiation of periosteal cells resulting in stable cartilage and bone formation in vivo.

Chondrogenic mesenchymal stem cells (MSCs) have not yet been used to address the clinical demands of large osteochondral joint surface defects. In this study, self-assembling tissue intermediates (TIs) derived from human periosteum-derived stem/progenitor cells (hPDCs) were generated and validated for stable cartilage formation in vivo using two different animal models.status: publishe

Integration of juvenile habitat quality and river connectivity models to understand and prioritise the management of barriers for Atlantic salmon populations across spatial scales

Thanks to the Scottish Government Hydro Nation Scholarship programme for funding WBB. Authors from Marine Scotland Science Freshwater Fisheries Laboratories delivered this work through Service Level Agreement FW02G. Some map features are based on digital spatial data licensed from CEH, NERC© Crown Copyright and database right (2018), all rights reserved. Ordnance Survey License number 100024655. Catchment boundaries were from SEPA (2009). The Obstacles to Fish Migration dataset is from SEPA. The authors thank the two anonymous referees for their feedback on the manuscript.Peer reviewedPostprin

Graviton emission in Einstein-Hilbert gravity

The five-point amplitude for the scattering of two distinct scalars with the emission of one graviton in the final state is calculated in exact kinematics for Einstein-Hilbert gravity. The result, which satisfies the Steinmann relations, is expressed in Sudakov variables, finding that it corresponds to the sum of two gauge invariant contributions written in terms of a new two scalar - two graviton effective vertex. A similar calculation is carried out in Quantum Chromodynamics (QCD) for the scattering of two distinct quarks with one extra gluon in the final state. The effective vertices which appear in both cases are then evaluated in the multi-Regge limit reproducing the well-known result obtained by Lipatov where the Einstein-Hilbert graviton emission vertex can be written as the product of two QCD gluon emission vertices, up to corrections to preserve the Steinmann relations.Comment: 28 pages, LaTeX, feynmf. v2: typos corrected, reference added. Final version to appear in Journal of High Energy Physic