growth pathway
Recently Published Documents


TOTAL DOCUMENTS

72
(FIVE YEARS 12)

H-INDEX

19
(FIVE YEARS 0)

Author(s):  
Hogeun Chang ◽  
Megalamane S. Bootharaju ◽  
Sanghwa Lee ◽  
Jeong Hyun Kim ◽  
Byung Hyo Kim ◽  
...  

2021 ◽  
Author(s):  
Roz Price

There has been a considerable amount of research generally into the benefits associated with low carbon development, showing that it can be synergistic with development priorities – such as job creation, improved public health, social inclusion and improved accessibility (see for example, Gouldson et al., 2018). However, this rapid review finds limited evidence and information around these benefits specifically for the Hashemite Kingdom of Jordan. There has been much interest in green growth in Jordan in the last ten years, particularly as Jordan is seen as having a large renewable energy potential for solar and wind. International organisations have been working with Jordan to develop comprehensive national plans and strategies to encourage green growth investment. Within the Jordanian government, the green growth concept has mainly been promoted by the Ministry of Environment. The World Bank in particular has produced a number of reports that have fed into this review, that explore or touch on green growth in Jordan – however, they themselves recognise that there is a lack of research on the economic and job-generating impacts of a green growth pathway in Jordan, and emphasise the need for further analysis (see specifically Hakim et al., 2017). Many of the green growth statistics referenced are from single reports undertaken a number of years ago – for example, that environmental degradation costs Jordan 2% of its GDP per year comes from a World Bank report written in 2010 and based on data from 2006 (World Bank, 2010). No more recent reviews were found during this rapid review. This review draws on a mixture of academic and grey literature from government and international organisations.


2020 ◽  
Vol 117 (40) ◽  
pp. 24701-24708
Author(s):  
Liwen Li ◽  
Jie Zhong ◽  
Youguo Yan ◽  
Jun Zhang ◽  
Jiafang Xu ◽  
...  

Methane clathrates are widespread on the ocean floor of the Earth. A better understanding of methane clathrate formation has important implications for natural-gas exploitation, storage, and transportation. A key step toward understanding clathrate formation is hydrate nucleation, which has been suggested to involve multiple evolution pathways. Herein, a unique nucleation/growth pathway for methane clathrate formation has been identified by analyzing the trajectories of large-scale molecular dynamics (MD) simulations. In particular, ternary water-ring aggregations (TWRAs) have been identified as fundamental structures for characterizing the nucleation pathway. Based on this nucleation pathway, the critical nucleus size and nucleation timescale can be quantitatively determined. Specifically, a methane hydration layer compression/shedding process is observed to be the critical step in (and driving) the nucleation/growth pathway, which is manifested through overlapping/compression of the surrounding hydration layers of the methane molecules, followed by detachment (shedding) of the hydration layer. As such, an effective way to control methane hydrate nucleation is to alter the hydration layer compression/shedding process during the course of nucleation.


ACS Omega ◽  
2020 ◽  
Vol 5 (29) ◽  
pp. 18441-18448
Author(s):  
Yi-Hsin Liu ◽  
Ho-Ying Chen ◽  
Hsiu-Fang Fan ◽  
Yu-Hsien Chen ◽  
Fudong Wang

2020 ◽  
Author(s):  
Dylan Suvlu ◽  
Mohsen Farshad ◽  
Jayendran C. Rasaiah

We describe a model of nanocluster formation that incorporates competition between ligand adsorption and nanocluster growth. Growth occurs through the addition of a metal-ligand complex and coalescence of nanoclusters. The competition between ligands for binding sites on the nanoclusters and growth of the nanoclusters through coalescence creates interesting growth pathways. The patterns are reminiscent of those observed in the synthesis of gold thiolate nanoclusters. For a particular set of rate coefficients, described herein, we observe the formation of a kinetically stable nanocluster that participates in coalescent growth. This determines the size interval of the resulting nanoclusters in the size distribution. The kinetically stable cluster can be tuned by modifying the functional form of the number of surface sites on the nanoclusters, thereby changing the growth pathway and the final sizes of the clusters.


2020 ◽  
Author(s):  
Dylan Suvlu ◽  
Mohsen Farshad ◽  
Jayendran C. Rasaiah

We describe a model of nanocluster formation that incorporates competition between ligand adsorption and nanocluster growth. Growth occurs through the addition of a metal-ligand complex and coalescence of nanoclusters. The competition between ligands for binding sites on the nanoclusters and growth of the nanoclusters through coalescence creates interesting growth pathways. The patterns are reminiscent of those observed in the synthesis of gold thiolate nanoclusters. For a particular set of rate coefficients, described herein, we observe the formation of a kinetically stable nanocluster that participates in coalescent growth. This determines the size interval of the resulting nanoclusters in the size distribution. The kinetically stable cluster can be tuned by modifying the functional form of the number of surface sites on the nanoclusters, thereby changing the growth pathway and the final sizes of the clusters.


2020 ◽  
Author(s):  
Dylan Suvlu ◽  
Mohsen Farshad ◽  
Jayendran C. Rasaiah

We describe a model of nanocluster formation that incorporates competition between ligand adsorption and nanocluster growth. Growth occurs through the addition of a metal-ligand complex and coalescence of nanoclusters. The competition between ligands for binding sites on the nanoclusters and growth of the nanoclusters through coalescence creates interesting growth pathways. The patterns are reminiscent of those observed in the synthesis of gold thiolate nanoclusters. For a particular set of rate coefficients, described herein, we observe the formation of a kinetically stable nanocluster that participates in coalescent growth. This determines the size interval of the resulting nanoclusters in the size distribution. The kinetically stable cluster can be tuned by modifying the functional form of the number of surface sites on the nanoclusters, thereby changing the growth pathway and the final sizes of the clusters.


2020 ◽  
Vol 12 (37) ◽  
pp. 4534-4540
Author(s):  
Xinxin Sang ◽  
Qijun Zha ◽  
Xiangdao Nie ◽  
Dongyin Liu ◽  
Yansong Guo ◽  
...  

CNTs@UiO-66-NH2 hybrids prepared through an interfacial in situ growth pathway exhibited a high adsorption capacity 392 mg g−1 towards MO and can effectively separate the MO/MB mixture.


2020 ◽  
Vol 7 (1) ◽  
pp. 191619
Author(s):  
Zhihao Rong ◽  
Xincun Tang ◽  
Liping Wu ◽  
Xi Chen ◽  
Wei Dang ◽  
...  

In this study, we propose a growth pathway of scorodite in an atmospheric scorodite synthesis. Scorodite is a non-direct product, which is derived from the transformation of its precursor. Different precursor speciation leads to different crystallinity and morphology of synthesized scorodite. At 10 and 20 g l −1 initial arsenic concentration, the precursor of scorodite is identified as ferrihydrite. At 10 g l −1 initial arsenic concentration, low arsenic concentration is unfavourable to the complex between arsenate and ferrihydrite, inhibiting the transformation of ferrihydrite into scorodite. The synthesized scorodite is 1–3 µm in size. At 20 g l −1 initial arsenic concentration, higher arsenic concentration favours the complex between arsenate and ferrihydrite. The transformation process is accessible. Large scorodite in the particle size of 5–20 µm with excellent crystallinity is obtained. However, the increasing initial arsenic concentration is not always a positive force for the growth of scorodite. When initial arsenic concentration increases to 30 g l −1 , Fe(O,OH) 6 octahedron preferentially connects to As(O,OH) 4 tetrahedron to form Fe H 2 As O 4 2 + or FeHAs O 4 + ion. Fe–As complex ions accumulate in solution. Once the supersaturation exceeds the critical value, the Fe–As complex ions deprotonate and form poorly crystalline ferric arsenate. Even poorly crystalline ferric arsenate can also transform to crystalline scorodite, its transformation process is much slower than ferrihydrite. Therefore, incomplete developed scorodite with poor crystallinity is obtained.


Sign in / Sign up

Export Citation Format

Share Document