Mesoscopic and macroscopic investigation of a dolomitic marble subjected to thermal damage.

Thermal loading is an important factor that could lead to the weakening and deterioration of rock materials. Understanding the thermal properties of rocks and their evolution under different high temperatures is important in the post-fire-hazard evaluation and cultural heritage conservation. Yet it is challenging to understand the evolution of thermally-induced changes in rock properties and to quantitatively study degrees of thermal damage when samples are limited. This study investigates the effects of high temperatures (i.e., 200 °C, 400 °C, 600 °C, 800 °C, and 1000 °C) on a dolomitic marble using combined mesoscopic and macroscopic testing techniques. The test results show that increasing marble temperature led to a deterioration of physical properties (i.e., increasing open porosity and weight loss; but decreasing P-wave velocity) and mechanical properties (i.e., increasing axial strain corresponding with the peak stress; but decreasing uniaxial compressive strength, Young's modulus, and brittleness). There existed a threshold temperature of 600 °C, which marks different thermal damage mechanisms. Below the threshold, the rock deterioration was mainly caused by physical changes such as crack propagation and grain breakage, which can be characterized by mesoscopic parameters (i.e., linear crack density and mineral grain size distribution). On the contrary, when the temperature was higher than the threshold, the deterioration was caused by chemical changes, including mineral decomposition and re-crystallization, which was indicated by the changes in mineral compositions and relative atomic mass calculation. Based on the experimental results (e.g., mineralogical and physico-mechanical changes) and obtained relationships between the parameters in mesoscale and macroscale, a novel scheme for thermal damage evaluation is proposed to estimate thermally-induced changes in macroscopic parameters (e.g., Young's modulus) based on the corresponding mesoscopic parameters (e.g., particle size distribution and linear crack density).

Characteristics and weathering mechanisms of the traditional Chinese blue brick from the ancient city of Ping Yao.

The traditional blue brick was the dominant clay brick used in Chinese architecture before the mid-nineteenth century. The ancient city of Ping Yao, a United Nations Educational, Scientific and Cultural Organization (UNESCO) heritage site, is an outstanding example of blue brick architecture. The Ping Yao bricks within the damp areas (up to 4 m at highest) of the ancient city's walls and private houses are subjected to various weathering, including contour scaling, flaking, powdering and salt crystallization. This study aims to characterize the properties, analyse weathering mechanisms, determine the main weathering factors and discuss the anti-weathering strategies of blue bricks. To do so, samples of brick and salt efflorescence were collected from the historical buildings of Ping Yao and were studied with regard to their mineralogical and physico-mechanical (e.g. density, porosity, pore size distribution, water absorption and uniaxial compressive strength) properties. The resistance to salt crystallization and frost, and the maximum firing temperatures of the brick samples were determined in the laboratory. Weathering mechanisms and anti-weathering strategies were discussed. Salt crystallization and freeze-thaw cycles were found to be two important factors that lead to brick weathering. An anti-weathering strategy of 'damp blocking, desalination and brick replacing' was discussed based on the laboratory experiments, suggestions in literature and site conditions.

An improved cellular enucleation method with extracellular matrix and colchicine facilitates the study of nucleocytoplasmic interaction.

Enucleated mammalian cells (cytoplasts) have been widely used for studying differential roles of the cytoplasm and nucleus in various cellular processes. Here, we reported an improved enucleation protocol, in which cells were seeded in extracellular matrix (ECM)-coated 24-wells and spun at 4600 g and 35 °C for 60 min in the presence of cytochalasin B and colchicine. When glass-bottom wells were used, cellular structures and organelles in cytoplasts could be examined directly by confocal microscopy. Nuclear envelope rupture did not occur probably due to mild centrifugation conditions used in this study. Addition of paclitaxel or doxorubicin completely blocked proliferation of residual nucleated cells; however, to our surprise, paclitaxel dramatically prolonged the survival of cytoplasts. Results from Annexin V and Propidium Iodide staining showed that cytoplasts died predominantly by apoptosis, which was partially inhibited by ECM and further by paclitaxel. Mitochondria were mostly rod-shaped and formed a connected network in paclitaxel-treated cytoplasts, indicating lack of fusion and fission dynamics. Moreover, paclitaxel increased mitochondrial membrane potential, suggesting that perturbation of mitochondria might be critical to the survival of cytoplasts. In conclusion, we had established an efficient and fast procedure for enucleation of adherent animal cells, which could facilitate the investigation of nucleocytoplasmic interaction.

Thermally induced deterioration behaviour of two dolomitic marbles under heating-cooling cycles.

Thermally induced deterioration behaviour can cause severe weathering in marbles. Most previous studies focus on the deterioration behaviour of calcitic marbles. Relevant studies of dolomitic marbles are generally carried out under a 'high temperature and low cycling times' condition. Little attention is focused on the deterioration behaviour in dolomitic marbles when they are subjected to a large quantity of heating-cooling cycles under a 'low temperature and high cycling times' condition. This paper presents experimental investigations on the thermally induced deterioration behaviour of two Beijing dolomitic marbles (Qingbaishi Marble (QM) and Hanbaiyu Marble (HM)) under heating-cooling cycles up to 1000 cycling times. The applied temperature range is from -20°C to 60°C which is to simulate the seasonal temperature variations in Beijing city, China. Related properties such as weight loss, three-dimensional microtopography, elastic wave velocity and uniaxial compressive strength were measured at certain cycles. The results indicate that thermally induced deterioration behaviour will result in a continuous weight loss in dolomitic marble samples. Mechanical properties of those two marbles are strongly affected by heating and cooling treatments, which were reflected by the reductions of dynamic Young's modulus and uniaxial compressive strength with an increase of thermal cycles. Compared with QM, HM displays a higher level of thermally induced deterioration which should be due to the abundance of quartz mineral.