Automated Author ProfileCall, Mitchell
Call, Mitchell
Current S-Index
Sum of Dataset Indices for all datasets
Average Dataset Index per Dataset
Average Dataset Index per dataset
Total Datasets
Total datasets for this author
Average FAIR Score
Average FAIR Score per dataset
Total Citations
Total citations to the author's datasets
Total Mentions
Total mentions of the author's datasets
S-Index Interpretation
The S-Index (Sharing Index) is a comprehensive metric that represents the cumulative impact of all your datasets. It is calculated as the sum of Dataset Index scores across all your claimed datasets.
What it means:
- A higher S-index indicates greater overall impact of your datasets relative to typical datasets in their fields of research
- The S-Index grows as you add more datasets or as existing datasets gain more citations and mentions
- It provides a single number to track your research data impact over time
Current S-Index: 2.3 (sum of 3 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
Here we report coupled, high resolution measurements of pCO2, CH4 and 222Rn during receding waters in the three major water types of the Central Amazon Basin: black (Negro River); clear (Tapajos River); white (Madeira River). Considerable spatial heterogeneity was observed in pCO2, CH4 and 222Rn concentrations ranging from 460 to 8030 uatm, 7 to 281 nM, and 713 to 8516 dpm m-3, respectively. the significant correlations between pCO2 and CH4 to 222Rn in the black and clear waters suggests that pore-water further enhanced CO2 supersaturation by 18 - 47 % and is a driver of CH4 dynamics in these waters.
Authors
- Call, Mitchell
Here we report coupled, high resolution measurements of pCO2, CH4 and 222Rn during receding waters in the three major water types of the Central Amazon Basin: black (Negro River); clear (Tapajos River); white (Madeira River). Considerable spatial heterogeneity was observed in pCO2, CH4 and 222Rn concentrations ranging from 460 to 8030 uatm, 7 to 281 nM, and 713 to 8516 dpm m-3, respectively. the significant correlations between pCO2 and CH4 to 222Rn in the black and clear waters suggests that pore-water further enhanced CO2 supersaturation by 18 - 47 % and is a driver of CH4 dynamics in these waters.
Authors
- Call, Mitchell
Here we report coupled, high resolution measurements of pCO2, CH4 and 222Rn during receding waters in the three major water types of the Central Amazon Basin: black (Negro River); clear (Tapajos River); white (Madeira River). Considerable spatial heterogeneity was observed in pCO2, CH4 and 222Rn concentrations ranging from 460 to 8030 uatm, 7 to 281 nM, and 713 to 8516 dpm m-3, respectively. the significant correlations between pCO2 and CH4 to 222Rn in the black and clear waters suggests that pore-water further enhanced CO2 supersaturation by 18 - 47 % and is a driver of CH4 dynamics in these waters.
Authors
- Call, Mitchell