41 research outputs found

    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

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    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

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    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

    Pore-Scale Investigation of CH<sub>4</sub> Hydrate Kinetics in Clayey-Silty Sediments by Low-Field NMR

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    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
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