41 research outputs found
Additional file 3: of Tau GSTs involved in regulation of leaf abscission by comparison the gene profiling of MeGSTs in various abscission-promoting treatments in cassava abscission zones
Figure S1. Sequence logos for conserved motifs identified in MeGSTs by MEME analysis. (JPG 1160 kb
Additional file 2: of Tau GSTs involved in regulation of leaf abscission by comparison the gene profiling of MeGSTs in various abscission-promoting treatments in cassava abscission zones
Data 2. The accession numbers of GSTs in cassava. (XLSX 20 kb
Additional file 2: of Genome-wide transcriptome analysis and identification of benzothiadiazole-induced genes and pathways potentially associated with defense response in banana
Table S1. The information of 3996 identified banana novel protein-coding transcripts in the study. (XLSX 4797 kb
Additional file 5: of Tau GSTs involved in regulation of leaf abscission by comparison the gene profiling of MeGSTs in various abscission-promoting treatments in cassava abscission zones
Data 4. Five clusters of the cassava GST genes expressed in abscission zones in ethylene treatment or drought treatment induced leaf abscission by Hierarchical clustering analysis. (XLS 36 kb
Additional file 3: of Genome-wide transcriptome analysis and identification of benzothiadiazole-induced genes and pathways potentially associated with defense response in banana
Table S2a. Expression information of DEGs in leaves at 1 day after BTH treatment. Table S2b. Expression information of DEGs in leaves at 3 day after BTH treatment. Table S2c. Expression information of DEGs in roots at 1 day after BTH treatment. Table S2d. Expression information of DEGs in roots at 3 day after BTH treatment. (XLSX 2340 kb
Additional file 6: of Genome-wide transcriptome analysis and identification of benzothiadiazole-induced genes and pathways potentially associated with defense response in banana
Table S5. Differentially expressed genes involved in protein kinases and transcription factors. (XLSX 225 kb
Additional file 5: of Genome-wide transcriptome analysis and identification of benzothiadiazole-induced genes and pathways potentially associated with defense response in banana
Table S4. The significantly enriched pathways of DEGs in banana leaves and roots. (XLSX 11 kb
Additional file 7: of Genome-wide transcriptome analysis and identification of benzothiadiazole-induced genes and pathways potentially associated with defense response in banana
Table S6. Expression information of DEGs in Figs. 5 and 6. (XLSX 123 kb
Additional file 1: of Tau GSTs involved in regulation of leaf abscission by comparison the gene profiling of MeGSTs in various abscission-promoting treatments in cassava abscission zones
Data 1. Primers used in qRT-PCR analysis. (XLS 39 kb
Pore-Scale Investigation of CH<sub>4</sub> Hydrate Kinetics in Clayey-Silty Sediments by Low-Field NMR
Clayey-silty sandy media have been widely discovered
in naturally
occurring hydrate-bearing sediments in the South China Sea. However,
the phase change behavior of CH4 hydrate (MH) and the resulting
pore structure change and the migration of fluid in clayey-silty sediments
remain less known and warrant investigation. In this study, we examine
the pore-scale behavior of MH formation and dissociation in clayey-silty
sediments and the associated fluid migration by low-field nuclear
magnetic resonance (NMR). Based on T2 spectra
measurement, MH starts to grow in small pores (pore size <1 μm)
first and in large pores (pore size >10 μm) subsequently.
The
presence of clay, i.e., Na-MMT, practically retards the overall growth
kinetics of MH evidenced by the low H2O conversion (<10%)
to MH in clay-associated small pores. During depressurization, MH
starts to dissociate in sand-associated large pores first. Free water
migrates to clay-associated small pores and partially converts to
clay-bound water. MRI visualization depicts the heterogeneous spatial
distribution of both MH and the residual water in the process. The
experimental results provide possible explanations on the spatial
heterogeneity of MH in clay-silty sediments in nature and on the multiphase
fluid migration during energy recovery from MH reservoirs