Source data - by Desheng Xie (21439869)

“…The results indicate that: 1) Vegetation cover in the affected regions decreased from 0.43 to 0.38 between 2017 and 2024, with Fire Zone 1 showing minimal recovery and Fire Zone 3 exhibiting moderate improvement, though the overall low vegetation area expanded due to ongoing fires; 2) The Remote Sensing Ecological Index (RSEI) declined from 0.41 to 0.38, with poor-rated areas increasing significantly, particularly in Fire Zone 3, reflecting the ongoing degradation of ecological conditions caused by both fire activity and climate factors; 3) The Flat Spectral Shape Index (FSSI) showed stability, but fluctuations in the areas with moderate and high probability of exposed coal, especially in Fire Zone 3, pointed to the expanding fire footprint and worsening ecological degradation; 4) Surface subsidence varied considerably, with Fire Zone 3 experiencing the most severe subsidence, indicating unstable geological conditions exacerbated by fire activity. …”

Contents of ions in the soil samples. by Fang Zheng (54278)

“…This phenomenon results in an “S” distribution of the salt content inside the SC. At the end of the freeze-thaw cycle (FTC), the deformation of the saline soil increased with the decrease of the cold end temperature, and the alternating time between heat and cold did not produce significant changes in the deformation of the saline soil. …”

Test scheme. by Fang Zheng (54278)

“…This phenomenon results in an “S” distribution of the salt content inside the SC. At the end of the freeze-thaw cycle (FTC), the deformation of the saline soil increased with the decrease of the cold end temperature, and the alternating time between heat and cold did not produce significant changes in the deformation of the saline soil. …”

Basic physical properties of the soil samples. by Fang Zheng (54278)

“…This phenomenon results in an “S” distribution of the salt content inside the SC. At the end of the freeze-thaw cycle (FTC), the deformation of the saline soil increased with the decrease of the cold end temperature, and the alternating time between heat and cold did not produce significant changes in the deformation of the saline soil. …”

Schematic diagram of WSM test simulator. by Fang Zheng (54278)

“…This phenomenon results in an “S” distribution of the salt content inside the SC. At the end of the freeze-thaw cycle (FTC), the deformation of the saline soil increased with the decrease of the cold end temperature, and the alternating time between heat and cold did not produce significant changes in the deformation of the saline soil. …”

Test device for WSM. by Fang Zheng (54278)

“…This phenomenon results in an “S” distribution of the salt content inside the SC. At the end of the freeze-thaw cycle (FTC), the deformation of the saline soil increased with the decrease of the cold end temperature, and the alternating time between heat and cold did not produce significant changes in the deformation of the saline soil. …”

Supporting data. by Fang Zheng (54278)

“…This phenomenon results in an “S” distribution of the salt content inside the SC. At the end of the freeze-thaw cycle (FTC), the deformation of the saline soil increased with the decrease of the cold end temperature, and the alternating time between heat and cold did not produce significant changes in the deformation of the saline soil. …”

Flow chart of the sample preparation process. by Fang Zheng (54278)

“…This phenomenon results in an “S” distribution of the salt content inside the SC. At the end of the freeze-thaw cycle (FTC), the deformation of the saline soil increased with the decrease of the cold end temperature, and the alternating time between heat and cold did not produce significant changes in the deformation of the saline soil. …”

Particle size curve. by Fang Zheng (54278)

“…This phenomenon results in an “S” distribution of the salt content inside the SC. At the end of the freeze-thaw cycle (FTC), the deformation of the saline soil increased with the decrease of the cold end temperature, and the alternating time between heat and cold did not produce significant changes in the deformation of the saline soil. …”

Compaction curve. by Fang Zheng (54278)

“…This phenomenon results in an “S” distribution of the salt content inside the SC. At the end of the freeze-thaw cycle (FTC), the deformation of the saline soil increased with the decrease of the cold end temperature, and the alternating time between heat and cold did not produce significant changes in the deformation of the saline soil. …”

Molecular Insights into the Crystallization of 4’-Hydroxyacetophenone from Water: Solute Aggregation, Liquid–Liquid Phase Separation, and Polymorph Selection by Carlos E. S. Bernardes (7183481)

“…As cooling progresses, they become more compact, a process accompanied by a reduction in water content, which is more significant as the solution concentration increases. …”

Molecular Insights into the Crystallization of 4’-Hydroxyacetophenone from Water: Solute Aggregation, Liquid–Liquid Phase Separation, and Polymorph Selection by Carlos E. S. Bernardes (7183481)

“…As cooling progresses, they become more compact, a process accompanied by a reduction in water content, which is more significant as the solution concentration increases. …”

Molecular Insights into the Crystallization of 4’-Hydroxyacetophenone from Water: Solute Aggregation, Liquid–Liquid Phase Separation, and Polymorph Selection by Carlos E. S. Bernardes (7183481)

“…As cooling progresses, they become more compact, a process accompanied by a reduction in water content, which is more significant as the solution concentration increases. …”

Table1_The interaction between selenium and other elements in soil and rice roots shaped by straw and straw biochar regulated the enrichment of selenium in rice grain.docx by Qinlei Rong (3815335)

Image 1_Genotype-dependent response to water deficit: increases in maize cell wall digestibility occurs through reducing both p-coumaric acid and lignification of the rind.jpeg by Ana López-Malvar (3751006)

“…Notably, in plastic genotypes, increases in IVCWRD in response to water deficit were concomitant to reductions in p-coumaric acid content and a decrease in red-stained lignified tissues in the rind. …”

Image 2_Genotype-dependent response to water deficit: increases in maize cell wall digestibility occurs through reducing both p-coumaric acid and lignification of the rind.tif by Ana López-Malvar (3751006)

“…Notably, in plastic genotypes, increases in IVCWRD in response to water deficit were concomitant to reductions in p-coumaric acid content and a decrease in red-stained lignified tissues in the rind. …”

Supplementary file 1_Taxonomic and functional shifts in soil nematode communities following estuarine island reclamation.docx by Sufeng Pan (21460022)

“…We found a significant decrease in both taxonomic and functional diversity as tidal flats were converted to dry land, followed by a gradual recovery that progressed with increasing reclamation age. …”

Analyzing the chemical environment of bent bamboo (<i>Phyllostachys iridescens</i>) sections using XRD, XPS, and FTIR analysis by Xuehua Wang (1903936)

“…Chemical degradation varies on the thermal bent bamboo sections, the O/C ratio increases from 0.26 of MW to 0.36 of CW, accompanied a decrease in the C_ox/unox ratio from 0.93 of MW to 0.81 of VW. …”

Data_Sheet_1_Distribution characteristics of soil active organic carbon at different elevations and its effects on microbial communities in southeast Tibet.PDF by Fanglin Ran (19931256)

“…The Shannon diversity of bacteria exhibited a significant decrease with increasing altitude, whereas no significant change was observed in the diversity of fungi. …”

Table 1_Effects of vegetation restoration on soil fungi community structure and assembly process in a semiarid alpine mining region.docx by Yuanyuan Xue (6442661)

“…However, with prolonged restoration duration, we observed a significant decrease in α diversity accompanied by a corresponding increase in β diversity. …”