No abstract

Riverine dissolved inorganic carbon (DIC) exports play a central role in the regional and global carbon cycles. Here, we investigated the spatiotemporal variability and sources of DIC in eight catchments in the Yangtze River source region (YRSR) with variable permafrost coverage and seasonally thawed active layers. The YRSR catchments are DIC-rich (averagely 25 mg C L −1 ) and export 3.51 g m −2 yr −1 of DIC. The seasonal changes of temperature, active layer, flow path, and discharge can alter DIC and stable carbon isotope of DIC (δ 13 C-DIC). The most depleted δ 13 C-DIC values were found in the thawed period, suggesting the soil-respired CO 2 during the active layer thaw period can promote bicarbonate production via H 2 CO 3 weathering. Spatially, δ 13 C-DIC values increased downstream, likely due to CO 2 outgassing and changed permafrost coverage and runoff. We found that evaporite dissolution and silicate weathering in the seasonally thawed active layer contributed 44.2% and 30.9% of stream HCO 3 -, respectively, while groundwater and rainwater contributed 16.7% and 7.3% of HCO 3 -, respectively. Pure carbonate rock weathering played a negligible role in DIC production. These results were compatible with δ 13 C-DIC source approximation results. Silicate weathering increased from initial thaw to thawed period, reflecting the active layer thaw and subsequent hydrology change impacts. Silicate weathering consumed 1.25 × 10 10 mol of CO 2 annually, while evaporite dissolution may produce CO 2 and neutralize this CO 2 sink. This study provides new understanding of the riverine DIC export processes of the YRSR. As permafrost degrades, the quantity, sources, and sinks of riverine DIC may also change spatiotemporally.

In the present work, the injection-molded poly­(l-lactide)/poly­(d-lactide) parts were thermally treated at nearly below the melting point of stereocomplex crystals (SCs) (∼210 °C) to prepare polylactides (PLAs) with good heat resistance, and it is found that exclusive formation of SC is effectively achieved. It is worth mentioning that injection-molded PLAs used in thermal treatment were first prepared by employing a high mold temperature (120 °C) to ensure proper crystallinity and SC content, which makes sure that no warpage of PLA was noticed during thermal treatment. Consequently, superbly heat resistant injection-molded parts with Vicat softening temperature of ∼200 °C were successfully achieved. Meanwhile, the template effect of residual SCs, as evidenced by in situ X-ray diffraction results, was proposed to explain the high efficiency of thermal treatment. Specifically, the residual SC in PLA melts with perfect surface and well-defined lattice parameters can act as template to guide formation of new SCs.