ALBERT

Description: Conventional spectral-based classification methods have significant limitations in the digital classification of urban land-use and land-cover classes from high-resolution remotely sensed data because of the lack of consideration given to the spatial properties of images. To recognize the complex distribution of urban features in high-resolution image data, texture information consisting of a group of pixels should be considered. Lacunarity is an index used to characterize different texture appearances. It is often reported that the land-use and land-cover in urban areas can be effectively classified using the lacunarity index with high-resolution images. However, the applicability of the maximum-likelihood approach for hybrid analysis has not been reported. A more effective approach that employs the original spectral data and lacunarity index can be expected to improve the accuracy of the classification. A new classification procedure referred to as “gradable classification method” is proposed in this study. This method improves the classification accuracy in incremental steps. The proposed classification approach integrates several classification maps created from original images and lacunarity maps, which consist of lacnarity values, to create a new classification map. The results of this study confirm the suitability of the gradable classification approach, which produced a higher overall accuracy (68%) and kappa coefficient (0.64) than those (65% and 0.60, respectively) obtained with the maximum-likelihood approach.

Description: Minerals, Vol. 7, Pages 123: Electron Microscopy Observation of Biomineralization within Wood Tissues of Kurogaki Minerals doi: 10.3390/min7070123 Authors: Kazue Tazaki Atsuko Fukuyama Fumie Tazaki Teruaki Takehara Keiichi Nakamura Masayuki Okuno Yumiko Hashida Shozo Hashida Interactions between minerals and microorganisms play a crucial role in living wood tissues. However, living wood tissues have never been studied in the field. Fortunately, we found several kurogaki (black persimmon; Diospyros kaki) trees at Tawara in Kanazawa, Ishikawa, Japan. Here, we report the characterization of kurogaki based on scanning electron microscopy equipped with energy-dispersive spectroscopy (SEM-EDS) and transmission electron microscopy (TEM), associated with inductively coupled plasma-mass spectrometry (ICP-MS) analyses, X-ray fluorescence analyses (XRF) and X-ray powder diffraction (XRD) analyses. This study aims to illustrate the ability of various microorganisms associated with biominerals within wood tissues of kurogaki, as shown by SEM-EDS elemental content maps and TEM images. Kurogaki grows very slowly and has extremely hard wood, known for its striking black and beige coloration, referred to as a “peacock pattern”. However, the scientific data for kurogaki are very limited. The black “peacock pattern” of the wood mainly comprises cellulose and high levels of crystal cristobalite. As per the XRD results, the black taproot contains mineralized 7 Å clays (kaolinite), cellulose, apatite and cristobalite associated with many microorganisms. The chemical compositions of the black and beige portions of the black persimmon tree were obtained by ICP-MS analyses. Particular elements such as abundant Ca, Mg, K, P, Mn, Ba, S, Cl, Fe, Na, and Al were concentrated in the black region, associated with Pb and Sr elements. SEM-EDS semi-qualitative analyses of kurogaki indicated an abundance of P and Ca in microorganisms in the black region, associated with Pb, Sr, S, Mn, and Mg elements. On the other hand, XRF and XRD mineralogical data showed that fresh andesite, weathered andesite, and the soils around the roots of kurogaki correlate with biomineralization of the black region in kurogaki roots, showing clay minerals (kaolinite) and cristobalite formation. In conclusion, we describe how the biominerals in the black region in the cellulose within wood tissues grow chemically and biologically in the sap under the conditions associated with the beige portions of the taproot. This can explain why the crystals produce the “peacock pattern” in the kurogaki formed during the year. We conclude that kurogaki microbiota are from bacteria in the andesitic weathered soil environment, which produce silicification. In other words, the patterned portions of kurogaki consist of silicified wood.

Description: Minerals, Vol. 8, Pages 178: Twenty Years after the Nakhodka Oil Spill Accident in the Sea of Japan, How Has Contamination Changed? Minerals doi: 10.3390/min8050178 Authors: Kazue Tazaki Atsuko Fukuyama Fumie Tazaki Yoshiaki Shintaku Keiichi Nakamura Teruaki Takehara Yoshihiro Katsura Keisuke Shimada The Nakhodka, a Russian tanker loaded with 19,000 kL of C-type heavy oil, was broken up into sections and submerged off Oki Island, Shimane Prefecture, Japan on 2 January 1997. The bow, after drifting for four days, was wrecked off Anto, Sakai City (Mikuni), Fukui Prefecture, threatening the environment throughout the various shores of Ishikawa Prefecture. The accident, caused by a heavy oil spill of 6200 kL, created serious environmental problems along the shores of Hokuriku District. We report the characterization of C-type heavy oil 20 years after the accident at the Atake seashore, Wajima City, Ishikawa Prefecture, in the Sea of Japan, based on observations in the field on 18 January 2017. We studied the microstructure, mineralogy, chemical composition, and radioactivity associated with microorganisms in the soils, and buried fishing nets and ropes that were contaminated with C-type heavy oil from this spill. The analyses used a combination of micro techniques, analytical data based on a CHN analyzer, X-ray powder diffraction (XRD), and two kinds of scanning electron microscopy equipped with energy dispersive spectroscopy (SEM-EDS). Hydrocarbon-degrading bacteria, paraffin wax, cristobalite, graphite, calcite, halite, and biotite from the Nakhodka oil spill were recognized on the surface of ropes and in the soil of the polluted seashores after 20 years. The chemical compositions indicated that high concentrations of C, O, Na, Al, Si, P, S, Ca, Fe, Cl, Sr, and Pb were predominantly indigenous to the Nakhodka oil spill. In the XRD analysis of the oil-contaminated soils on the rope at the Atake seashore indicated paraffin wax, graphite, sulfate, calcite and halite refractions with clay minerals, after 20 years. To date, no report has described the results of electron microscopy observations, such as Micrococcus bacillus and filamentous fungi, found in oil-contaminated soils after 20 years. In this research, such observations are introduced as “bioremediation” by hydrocarbon-degrading bacteria, graphite, and paraffin wax. On 18 January 2017, the reflection of graphite, paraffin wax, sulfur, calcite, and halite with clay minerals confirmed the occurrence of bioremediation. Many kinds of hydrocarbon-degrading microorganisms—such as filamentous fungi—were found in oil-contaminated soils after 20 years. We have used SEM-EDS to show semi-permanent bioremediation and biomineralization processes after 20 years.

Description: Minerals, Vol. 8, Pages 242: Mineralogical and Elemental Composition of Pectinatella magnifica and Its Statoblasts Minerals doi: 10.3390/min8060242 Authors: Kazue Tazaki Atsuko Fukuyama Fumie Tazaki Masayuki Okuno Yumiko Hashida Shozo Hashida Teruaki Takehara Keiichi Nakamura Tomohiro Kato Several massive colonies of Pectinatella magnifica have been observed during the summer almost every year since 1974 in agricultural reservoir ponds and lakes with dirty freshwater environments in Ishikawa, Japan, which has posed serious environmental problems on the shores of Hokuriku District. We collected Pectinatella magnifica during the summer at Kahokugata Lake and Makiyama agricultural reservoir pond in June and July 2016. However, scientific data for the statoblasts of Pectinatella magnifica are limited. Our results for scanning electron microscopy equipped with energy-dispersive spectroscopy (SEM-EDS), inductively coupled plasma-mass spectrometry (ICP-MS), and X-ray powder diffraction (XRD) analyses of Pectinatella magnifica indicated immobilization of the chemical elements that were involved in the mass during the summer. We also reported the characterization of an invasive species of bryozoan (Pectinatella magnifica) in lakes and ponds in Ishikawa, Japan, based on field observations in 2016. We studied the microstructure, mineralogy, chemical composition, and radioactivity associated with these organisms, using a combination of micro-techniques, SEM-EDS, associated with ICP-MS, and XRD. This study aims to illustrate the capability of Pectinatella magnifica to produce minerals within statoblasts and gelatinous material. Obtained results may indicate forming quartz, palygorskite, dolomite, bischofite, pyrolusite, and pyrite, associated with native sulfur and copper in the statoblast. The mass of gelatinous material contains talc and vermiculite as well as non-crystalline phase. The mechanism of biomineral formation has important implications for water–mineral–organism or microorganism interactions both in lower drainage basin systems, such as Kahokugata Lake, and upper water areas, such as Makiyama agricultural reservoir pond. Many types with variety of sizes and shapes of bryozoan (Pectinatella magnifica) were found in lakes and ponds in Japan. The biomineralization systems will be made available for use not only in researching bryozoans (Pectinatella magnifica), but also for environmental change systems from upstream to downstream of the lake. To date, there have been no reports on related electron microscopy observations, including the real-life occurrence of “bioremediation”. These observations could lead to simple methods of removing statoblasts of the invasive alien species Pectinatella magnifica from agricultural and reservoir environments, because there was limited microbial immobilization of the ions during the winter.

Description: Spatial variation and temporal changes in ground subsidence over the Nobi Plain, Central Japan, are assessed using GIS techniques and ground level measurements data taken over this area since the 1970s. Notwithstanding the general slowing trend observed in ground subsidence over the plains, we have detected ground rise at some locations, more likely due to the ground expansion because of recovering groundwater levels and the tilting of the Nobi land mass. The problem of non-availability of upper-air meteorological information, especially the 3-dimensional water vapor distribution, during the JERS-1 observational period (1992–1998) was solved by applying the AWC (analog weather charts) method onto the high-precision GPV-MSM (Grid Point Value of Meso-Scale Model) water-vapor data to find the latter’s matching meteorological data. From the selected JERS-1 interferometry pair and the matching GPV-MSM meteorological data, the atmospheric path delay generated by water vapor inhomogeneity was then quantitatively evaluated. A highly uniform spatial distribution of the atmospheric delay, with a maximum deviation of approximately 38 mm in its horizontal distribution was found over the Plain. This confirms the effectiveness of using GPV-MSM data for SAR differential interferometric analysis, and sheds thus some new light on the possibility of improving InSAR analysis results for land subsidence applications.