The mean residence time of river water in the Canada Basin
Bibliographic record
Abstract
海水为 O-18， Ra-226 和 Ra-228 的大小从西方的北极海洋被收集。在水样品的河流量和海冰融化水的部分被使用三角洲 O-18-S-PO 估计 * 示踪剂系统。在加拿大盆的河水的吝啬的滞留时间基于在 Ra-228/Ra-226 之间的关系被计算)(A.R ) 并且在架和深海洋中的河流量的部分。我们的结果证明在加拿大盆的河流量部分比在架区域的那些显著地高，建议加拿大盆是为北极河水的一个主要存储区域。在 Chukchi 架和博福特架中的 Ra-228 活动集中从 0.16 ～ 1.22 Bq/m (3 )，比在低、中间的纬度为架报导的那些低，显示海冰融化水的效果。一种好积极线性关系在 Ra-228/Ra-226 之间被观察)(A.R ) 并且为架的河流量的部分流水，当时 Ra-228/Ra-226 )(A.R ) 在加拿大，盆在这根回归的线下面位于。低 Ra-228/Ra-226 )(A.R ) 在加拿大，盆在搬运到深海洋的架水期间被归功于到 Ra-228 腐烂。5.0-11.0 的滞留时间一在加拿大盆为河水被估计，它决定了表面在诺思大西洋添到河流量进北极海洋的时间反应。
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How this classification was reachedexpand
Full frame distilled prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.000 | 0.000 |
| Science and technology studies | 0.000 | 0.001 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.000 | 0.000 |
Machine scores (provisional)
The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.
Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one teacher head, not a consensus.
How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".