Sample collection from asteroid (162173) Ryugu by Hayabusa2: Implications for surface evolution.

The near-Earth asteroid (162173) Ryugu is thought to be a primitive carbonaceous object that contains hydrated minerals and organic molecules. We report sample collection from Ryugu's surface by the Hayabusa2 spacecraft on 21 February 2019. Touchdown images and global observations of surface colors are used to investigate the stratigraphy of the surface around the sample location and across Ryugu. Latitudinal color variations suggest the reddening of exposed surface material by solar heating and/or space weathering. Immediately after touchdown, Hayabusa2's thrusters disturbed dark, fine grains that originate from the redder materials. The stratigraphic relationship between identified craters and the redder material indicates that surface reddening occurred over a short period of time. We suggest that Ryugu previously experienced an orbital excursion near the Sun.

Hayabusa2 arrives at the carbonaceous asteroid 162173 Ryugu-A spinning top-shaped rubble pile.

The Hayabusa2 spacecraft arrived at the near-Earth carbonaceous asteroid 162173 Ryugu in 2018. We present Hayabusa2 observations of Ryugu's shape, mass, and geomorphology. Ryugu has an oblate "spinning top" shape, with a prominent circular equatorial ridge. Its bulk density, 1.19 ± 0.02 grams per cubic centimeter, indicates a high-porosity (>50%) interior. Large surface boulders suggest a rubble-pile structure. Surface slope analysis shows Ryugu's shape may have been produced from having once spun at twice the current rate. Coupled with the observed global material homogeneity, this suggests that Ryugu was reshaped by centrifugally induced deformation during a period of rapid rotation. From these remote-sensing investigations, we identified a suitable sample collection site on the equatorial ridge.

The geomorphology, color, and thermal properties of Ryugu: Implications for parent-body processes.

The near-Earth carbonaceous asteroid 162173 Ryugu is thought to have been produced from a parent body that contained water ice and organic molecules. The Hayabusa2 spacecraft has obtained global multicolor images of Ryugu. Geomorphological features present include a circum-equatorial ridge, east-west dichotomy, high boulder abundances across the entire surface, and impact craters. Age estimates from the craters indicate a resurfacing age of [Formula: see text] years for the top 1-meter layer. Ryugu is among the darkest known bodies in the Solar System. The high abundance and spectral properties of boulders are consistent with moderately dehydrated materials, analogous to thermally metamorphosed meteorites found on Earth. The general uniformity in color across Ryugu's surface supports partial dehydration due to internal heating of the asteroid's parent body.

The 1997 Mars Pathfinder Spacecraft Landing Site: Spillover Deposits from an Early Mars Inland Sea.

The Martian outflow channels comprise some of the largest known channels in the Solar System. Remote-sensing investigations indicate that cataclysmic floods likely excavated the channels ~3.4 Ga. Previous studies show that, in the southern circum-Chryse region, their flooding pathways include hundreds of kilometers of channel floors with upward gradients. However, the impact of the reversed channel-floor topography on the cataclysmic floods remains uncertain. Here, we show that these channel floors occur within a vast basin, which separates the downstream reaches of numerous outflow channels from the northern plains. Consequently, floods propagating through these channels must have ponded, producing an inland sea, before reaching the northern plains as enormous spillover discharges. The resulting paleohydrological reconstruction reinterprets the 1997 Pathfinder landing site as part of a marine spillway, which connected the inland sea to a hypothesized northern plains ocean. Our flood simulation shows that the presence of the sea would have permitted the propagation of low-depth floods beyond the areas of reversed channel-floor topography. These results explain the formation at the landing site of possible fluvial features indicative of flow depths at least an order of magnitude lower than those apparent from the analyses of orbital remote-sensing observations.

Critical behavior of a random diode network.

We study the percolation properties of a random diode network (RDN) which contains two kinds of directed bonds on a square lattice. This network is a special case of the random insulation-resistor-diode network. Both Monte Carlo simulations and series expansion for the percolation probability show that an estimated critical exponent, beta=0.1794+/-0.008, is different from known values for a conventional insulation-resistor-diode network. RDN belongs to neither the isotropic percolation universality class nor to the directed percolation universality, which we attribute to a difference of symmetry breakdown around the critical point.

Theophylline toxicity in a preterm infant: selected clinical aspects.

A case of parent-induced theophylline toxicity in a preterm infant is described. Despite a theophylline level of 97 mcg/ml no clinical seizure activity was apparent. Pharmacokinetic data suggested that use of oral activated charcoal may have enhanced drug clearance. Further study is necessary before such therapy can be routinely advocated. Additional clinical features are discussed, including avoidance of dosing errors through careful instruction of all caretakers prior to discharge.

Developmental pattern of gentamicin kinetics in very low birth weight (VLBW) sick infants.

Kinetic studies were carried out in 15 very low birth weight (VLBW) infants during three courses of gentamicin (G) therapy for suspected sepsis. All received two courses but only 6 required a third course. G dosage was 2.0 +/- 0.2 mg/kg/24 h for the first and second course and 2.5 mg/kg/12 h for the third course. G dosage was adjusted to maintain serum peak G concentration of 4-8 micrograms/ml and trough concentration of 0.5-2 micrograms/ml. On the third day of therapy, a 24-hour collection of urine for creatinine (C) and G concentrations was performed in 28 of 36 cases. G clearance and G elimination rate constant were calculated based on chronological age (CA) of less than or equal to 7 (I), 8-30 (II) and greater than or equal to 31 (III) days. The mean BW and GA were 1,002 +/- 206 g and 28.4 +/- 1.5 weeks, respectively. Mean CA for the starting of therapy for each course was the first day, 19 +/- 9 and 68 +/- 26 days of life, respectively. Mean serum G peak and trough concentrations were 5.9 +/- 1.1 and 1.6 +/- 0.6 micrograms/ml for the first; 5.7 +/- 1.2 and 1.3 +/- 0.6 micrograms/ml for the second; 5.1 +/- 0.8 and 1.1 +/- 0.6 micrograms/ml for the third course of therapy. Mean apparent volume of distribution of G were 0.53 +/- 0.10 liter/kg for the first and 0.50 +/- 0.11 liter/kg for the second and third courses. Mean clearances for the three CA groups were 6.4 +/- 1.9; 7.6 +/- 3.2; 24.1 +/- 8.0 ml/min/1.73 m2 for G and 6.4 +/- 2.2; 7.7 +/- 3.1; 23.3 +/- 8.8 for C with serum C of 1.3 +/- 0.4, 1.2 +/- 0.6 and 0.6 +/- 0.4 mg%, respectively. There were no statistically significant differences for serum C, G and C clearance between CA I and II but significant differences were found for the above between CA III vs. CA I and II (p less than 0.005). G clearance closely correlated with C clearance (r = 0.99, p less than 0.001). The elimination rate constant was significantly higher after 30 days of life when CA III is compared to CA I and II or combined (p less than 0.001). This study shows that during the first month of life, VLBW sick infants still have decreased renal function and poor G clearance, therefore, G should be given every 24 h and the dose be adjusted based on individual patient serum G levels.

Large-for-gestational-age neonates: anthropometric reasons for shoulder dystocia.

From 1960 to 1980 at Memorial Hospital Medical Center--Miller Children's Hospital, the mean birth weight for term-size neonates increased from 3381 to 3458 g inspite of increases in ethnic groups known to have smaller neonates. More significantly, the incidence of macrosomic neonates (birth weight greater than 4000 g) increased from 7.0 to 10.7%. Because of this marked increase in the incidence of neonatal macrosomia, prospective study was designed to characterize the macrosomic neonate anthropometrically. The results of this study revealed that neonates experiencing shoulder dystocia had significantly greater shoulder-to-head and chest-to-head disproportions than did macrosomic neonates delivered by cesarean section for failed progress in labor or macrosomic neonates delivered without shoulder dystocia. In addition, neonates of diabetic mothers also showed significantly greater shoulder-head and chest-head size differences than did neonates of nondiabetic mothers of comparable weight. These data suggest that antenatal ultrasonic measurements to compare chest-head size difference in fetuses suspected to be macrosomic and in diabetic pregnancies could be of value in selecting patients for the appropriate route of delivery.