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| 1 | “Dietary fibre”: moving beyond the “soluble/insoluble” classification for monogastric nutrition, with an emphasis on humans and pigs显示文摘This review describes dietary fibres originating from a range of foods,particularly in relation to their plant cell walls.It explores the categorization of dietary fibres into 'soluble' or 'insoluble'.It also emphasizes dietary fibre fermentability,in terms of describing how the gastro-intestinal tract(GIT) microbiota respond to a selection of fibres from these categories.Food is categorized into cereals,legumes,fruits and vegetables.Mention is also made of example whole foods and why differences in physico-chemical characteristics between 'purified' and 'non-purified'food components are important in terms of health.Lastly,recommendations are made as to how dietary fibre could be classified differently,in relation to its functionality in terms of fermentability,rather than only its solubility. | Barbara A.Williams Deirdre Mikkelsen Bernadine M.Flanagan Michael J.Gidley | 2019 | Journal of Animal Science and Biotechnology2019，10，3： | 5 |
| 2 | Arsenic variability and groundwater age in three water supply wells in southeast New Hampshire显示文摘Three wells in New Hampshire were sampled bimonthly over three years to evaluate the temporal variability of arsenic concentrations and groundwater age.All samples had measurable concentrations of arsenic throughout the entire sampling period and concentrations in individual wells had a mean variation of more than 7 μg/L.The time series data from this sampling effort showed that arsenic concentrations ranged from a median of 4 mg/L in a glacial aquifer well (SGW-65) to medians of 19 μg/L and 37 μg/L in wells (SGW-93 and KFW-87) screened in the bedrock aquifer,respectively.These high arsenic concentrations were associated with the consistently high pH (median ≥- 8) and low dissolved oxygen (median <0.1 mg/L) in the bedrock aquifer wells,which is typical of fractured crystalline bedrock aquifers in New Hampshire.Groundwater from the glacial aquifer often has high dissolved oxygen,but in this case was consistently low.The pH also is generally acidic in the glacial aquifer but in this case was slightly alkaline (median =7.5).Also,sorption sites may be more abundant in glacial aquifer deposits than in fractured bedrock which may contribute to lower arsenic concentrations.Mean groundwater ages were less than 50 years old in all three wells and correlated with conservative tracer concentrations,such as chloride;however,mean age was not directly correlated with arsenic concentrations.Arsenic concentrations at KFW-87 did correlate with water levels,in addition,there was a seasonal pattern,which suggests that either the timing of or multiple sampling efforts may be important to define the full range of arsenic concentrations in domestic bedrock wells.Since geochemically reduced conditions and alkaline pHs are common to both bedrock and glacial aquifer wells in this study,groundwater age correlates less strongly with arsenic concentrations than geochemical conditions.There also is evidence of direct hydraulic connection between the glacial and bedrock aquifers,which can influence arsenic concentrations.Correlations between arsenic concentrations and the age of the old fraction of water in SGW-65 and the age of the young fraction of water in SGW-93 suggest that water in the two aquifers may be mixing or at least some of the deeper,older water captured by the glacial aquifer well may be from a similar source as the shallow young groundwater from the bedrock aquifer.The contrast in arsenic concentrations in the two aquifers may be because of increased adsorption capacity of glacio-fluvial sediments,which can limit contaminants more than fractured rock.In addition,this study illustrates that long residence times are not necessary to achieve more geochemically evolved conditions such as high pH and reduced conditions as is typically found with older water in other regions. | Joseph P.Levitt James R.Degnan Sarah M.Flanagan Bryant C.Jurgens | 2019 | Geoscience Frontiers2019，10，5： | 2 |
| 3 | Visual impairment in childhood: insights from a community‐based survey显示文摘 | N. M.Flanagan A. J.Jackson A. E.Hill | 2003 | Child: Care, Health and Development2003，，6： | 1 |
| 4 | 给自己的一封信:亲爱的老爸,你全都做错啦显示文摘亲爱的老爸:你全都做错啦。十一年前,医生们递给你一个包着脆弱小人儿的粉红小包裹。那时的你才26岁,走出医院后却要完完全全地对一个全新的人类生命负责——一个完完整整的人。似乎让你做那样的事是完全合乎情理的,但你却被吓坏了。最终,他们又交给你另外两个小人儿。按理说,像应该会依次变得轻松一点儿。但你没有。你的恐惧从未减少。对于如何当一个父亲你也从来没有什么把握。于是你决定,边学边做。你不用对此惑到难过——其他人也是这样做的。问题是,你总是听你周围的声音,却不去聆听发自内心深处的那个声音。对于这一点,你也可以原谅自己。毕竟,你周围的声音是那么大,又那么让人难以忽视。 | Kelly M.Flanagan 箐舞 | 2015 | 疯狂英语(初中天地)2015，0，8： | 0 |
| 5 | 亲爱的爸爸,你全都做错了显示文摘也许有时候爸爸太过急躁,也许有时候爸爸太过强硬,也许有时候爸爸太过笨拙,也许有时候爸爸太过……也许,还有许多地方爸爸做得并不够好。但是,透过下面这封爸爸的自责信,你或许会发现爸爸有一点确信无疑做得够好,那就是——他爱我们,从不曾改变,从不会改变。亲爱的爸爸:你全都做错了。11年前,医生们将一个小小的粉红色襁褓交到你手中,里面裹着一个脆弱的生命。那时你26岁,你走出医院,从此要为一个全新的小生命、一个完完整整的人负起全部责任。 | Kelly M.Flanagan 张玲 | 2015 | 新东方英语(中学版)2015，0，6： | 0 |
| 6 | 你全都做错了显示文摘亲爱的爸爸:
你全都做错了。
11年前,医生们将一个小小的粉红色襁褓交到你手中,里面裹着一个脆弱的生命。那时你26岁,你走出医院,从此要为一个全新的小生命、一个完完整整的人负起全部责任。这让你心生恐惧。 | Kelly M.Flanagan 张玲 | 2015 | 高中生(作文)2015，0，10： | 0 |
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