Ischiofemoral distances on supine and standing hip radiographs had good diagnostic performance and can be used as a screening tool, with optimal cutoff points.

No abstract

The carbon emissions and removals due to land cover changes between 2001 and 2010 in the Vu Gia Thu Bon River Basin, Central Vietnam, were estimated using Landsat satellite images and 3083 forest inventory plots. The net emissions from above-and belowground vegetation biomass were equal to 1.76 § 0.12 Tg CO 2 , about 1.1% of the existing stocks. The vast majority of carbon emissions were due to forest loss, with the conversion of forest to cropland accounting for 67% of net emissions. Forest regrowth had a substantial impact on net carbon changes, removing 22% of emissions from deforestation. Most deforestation occurred in regrowth forest (60%) and plantations (29%), characterized by low carbon stock density. Thus identifying the type of forest where deforestation occurred and using local field data were critical with net emissions being 4 times larger when considering only one forest class with average carbon stock, and 5-7 times higher when using literature default values or global emission maps. Carbon emissions from soil (up to 30 cm) were estimated for the main land change class. Due to the low emission factors from biomass, soils proved a key emission category, accounting for 30% of total land emissions that occurred during the monitoring period.

This study аims to explore cement leаkаge аs а complication of percutаneous vertebroplаsty (PVP) in the treаtment of multiple osteoporotic vertebrаl compression frаctures (MOVF). Patients and Methods: This prospective study wаs cаrried out on 32 consecutive pаtients with osteoporotic frаctures of аt leаst two vertebrаe (VB). Аll pаtients were over 50 yeаrs old аnd women аccounted for 29 out of the 32 pаtients (90.6%). PVP wаs performed under digitаl subtrаction аngiogrаphy (DSА) of аt leаst three VB, аnd 97 collаpsed VB аnd 105 VB were exаmined by PVP. Аll pаtients hаd postoperаtive computerized tomogrаphy (CT) to diаgnose аnd clаssify the complicаtions. Results: One hundred аnd five vertebrаe were exаmined with PVP, аnd 36/105 (34.3%) exhibited complicаtions of cement leаkаge. Type B cement leаkаge wаs the most common complicаtion, with 19/105 (18.1%) cаses; type C аccounted for 8/105 (7.6%) cаses; аnd type S аccounted for 9/105 (8.6%) cаses. There wаs only one (0.95%) cаse of cement leаkаge moving to the pulmonаry аrtery. Аll complicаtions hаd no clinicаl symptoms аnd did not require treаtment. Conclusion: Cement leаkаge is quite а common complicаtion, but it usuаlly hаs no clinicаl symptoms аnd does not require treаtment. Therefore, PVP is а sаfe аnd successful technique for the treаtment of multiple osteoporotic vertebrаl compression frаctures.

The sediment regime of the Red River system has changed since dams and reservoirs were implemented, with implications for river processes downstream. We analyzed data for the daily discharge (Q) and suspended particulate matter (SPM) concentrations collected from 1958–2021 at the Son Tay hydrological gauging station, the outlet of the Red River system and entry to the delta. The results showed that the annual sediment load transported by the Red River system decreased significantly, by about 90.4%, over the 64-year study period. From 1958 to 1971, when there were no dams or reservoirs in place, the annual water discharges and sediment loads in the river system were about 115,592×106 m3/yr and 115×106 ton/yr, respectively. From 1971 to 2016, a series of dam-reservoir systems were gradually implemented (Thac Ba (1971), Hoa Binh (1988), Tuyen Quang (2008), Son La (2010), Ban Chat (2013), Huoi Quang (2015), and Lai Chau (2016)). By 2016, the annual sediment load and water discharges in the Red River system had decreased significantly, and were 9×106 ton/yr and 88,709×106 m3/yr, respectively. The data show that the discharge and sediment loads increased slightly from 2016–2021, perhaps reflecting the combined effects of human activities, such as land-use change, deforestation, and population increases. Climate may also have played a role in these increases, with changes in air temperature and increases in rainfall triggering severe soil erosion and large discharges of sediment into the Red River system.