B Elemental contents of beach rock samples were analyzed using EDXRF.The samples were collected from three locations of Andaman Island.The Al,Ca,K,Fe,Ti,Si,V,Co,Cu,Ba,Zn,Pb,Cd and Mn contents were determined.The geoch...B Elemental contents of beach rock samples were analyzed using EDXRF.The samples were collected from three locations of Andaman Island.The Al,Ca,K,Fe,Ti,Si,V,Co,Cu,Ba,Zn,Pb,Cd and Mn contents were determined.The geochemical behavior of elements in the region is discussed.The elemental contents of beach rock samples from Andaman Island are much below the values of both earth crust and that of Tamilnadu region.However,content of the biogenic element Ca was the highest of all elements.This is due to the typical beach rock formation.展开更多
Beach rocks samples were collected from South East Coast of Tamilnadu, India. The mineralogical composition was determined using FT-IR and XRD. The natural radioactive measurements to detect radioactive elements were ...Beach rocks samples were collected from South East Coast of Tamilnadu, India. The mineralogical composition was determined using FT-IR and XRD. The natural radioactive measurements to detect radioactive elements were determined by gamma ray spectrometer. The multi-element analyses were carried out by INAA (Instrumental neutron activation analysis), with the standard Estuarine Sediment as reference material. The geochemical behavior of elements in the region is discussed. The occurrence of the radioactive and non-radioactive elements is discussed for their geological significance. The results were used to assess environmental toxicity of heavy metals and radiation hazard in the study area.展开更多
Element profiles of some beach rock samples collected from South East Coast of Tamilnadu, India have been determined using single comparator method of INAA. The geo-chemical behavior of the elements in the region is d...Element profiles of some beach rock samples collected from South East Coast of Tamilnadu, India have been determined using single comparator method of INAA. The geo-chemical behavior of the elements in the region is discussed. The irradiations were done at thermal neutron flux of ~ 1011 cm-2·s-1 at 20kW power using Kalpakkam Mini Reactor (KAMINI), IGCAR, Kalpakkam, Tamilnadu, India. Around 19 elements have been determined from 15 samples by high-resolution gamma spectrometry. The accuracy and precision were evaluated by assaying the irradiated Standard Reference Material (SRM 1646a Estuarine sediment) and were found to be in good agreement with certified values.展开更多
Beach rock,which forms at the intertidal zone,is a natural barrier to protect beach and island from wave erosion. The formation mechanism of beach rocks is significant in the study of surface carbonate diagenesis and ...Beach rock,which forms at the intertidal zone,is a natural barrier to protect beach and island from wave erosion. The formation mechanism of beach rocks is significant in the study of surface carbonate diagenesis and protection of island. Beach rocks in Qilian Islets and Cays were formed about 500–700 a BP,neither its composition nor sedimentary structure experienced intense post-reformation.Beach rocks in Qilian Islets and Cays are mainly composed of reef-building skeletal fragments and bioclasts without terrigenous sediments. This study focused on the types and morphologies of cements in beach rocks of Qilian Islets and Cays,and its cementation mechanisms and influencing factors. Biological activities,such as micritization caused by microbial activities and algae binding action,play an important role in the initial stage of bioclast transformation and promote the subsequent early marine and early meteoric cementation. Acicular aragonite induced by early marine cementation is well developed in beach rocks,especially in those samples from Medium Islet. Early meteoric cementation is not common as marine cementation,generally presenting granular and meniscus cements. The main factors affecting the formation and development of beach rocks in Qilian Islets and Cays include sediment source,hydrodynamic condition,climate,sea level change and anthropogenic impacts.展开更多
The formation of beach rocks has a close relationship to storm deposits, denoted by beach and storm processes in association with depositional characteristics of the beach rocks found in Pui O and Lower Cheung Sha bay...The formation of beach rocks has a close relationship to storm deposits, denoted by beach and storm processes in association with depositional characteristics of the beach rocks found in Pui O and Lower Cheung Sha bays on the southern coast of Lantau Island, Hong Kong. Although not all beach rocks have an origin of storm deposits, it is certain that some of them with very coarse shells and shell fragments developing on sandy beaches originate from storm deposits. The cementation of beach rocks on a beach was affected directly by the texture and structure of the beach rocks and wave energy varying along the beach.展开更多
Dune riocks are aeolian sands cemented ty calcium carbonate under subaerial conditions. They have been found in many of the coastal belts of Fujian, Guangdong and Hainan Provinces in South China. The grain composition...Dune riocks are aeolian sands cemented ty calcium carbonate under subaerial conditions. They have been found in many of the coastal belts of Fujian, Guangdong and Hainan Provinces in South China. The grain composition of the dune rocks is mainly quartz sands and shell fragments. The quartz sands are medium and fine sized, relatively well sorted and positively skewed. Their surface texture formed in aeolian environments is characterized ty dishshaped depressions, meniscus depressions and V-shaped depressions with rounded edges. The most common bedding type of the rocks is larg (thickness>1.5m), steeply dipping (32--40°) with cross strata tolaner and convex upward). Mg and Sr contents are very low in the rock chemical composition which is classified into low Mg and low Sr category. The typical species of microfossils in the dune rocks are mainly freshwater ones and lack of typical saltwaer or semi-saltwater ones with incomplete assemblage of marine species. The cement minerals in the rocks are mainly low-Mg calcite and the common cement fabrics are meniscus cement and gravitational cement in response to impermanent water in vadose zones. Therefore, the dune rocks may be apparently distinguished from the beach rocks.展开更多
The study investigates the potential of the serpulid tubeworm Ficopomatus sp.,sourced from Jesolo Lido(Venice,Italy),for CCS(Carbon Capture and Storage).Specimens were processed to extract bioactive compounds using a ...The study investigates the potential of the serpulid tubeworm Ficopomatus sp.,sourced from Jesolo Lido(Venice,Italy),for CCS(Carbon Capture and Storage).Specimens were processed to extract bioactive compounds using a 50%polypropylene glycol-water solvent system.Extracts were analysed and purified using column gel filtration chromatography,with fractions identified by TLC(Thin Layer Chromatography)and further characterized for antioxidant and antibacterial activities.Antioxidant activity was detected via DPPH(2,2-Diphenyl-1-Picrylhydrazyl)spraying on TLC plates,while antibacterial activity was evaluated using the antibiogram paper disk diffusion method.Enzyme activity in the fractions was previously confirmed through a bromothymol blue test followed by spectrophotometric analysis.The primary goal was to explore the CCS potential,using an experimental module involving Arduino Uno embedded microprocessor for the CO_(2) measurement and to confirm the conversion into insoluble carbonates(storage).The most active fraction,identified as S1,showed significant CCS action,confirmed by microscopic observation of calcareous deposits on treated sponges.These findings suggest that Ficopomatus sp.can be used in CCS research highlighting its potential for biotechnological applications in mitigating climate change.The paper underscores the importance of marine organisms in CCS and offers insights into innovative strategies for environmental conservation and carbon management.展开更多
文摘B Elemental contents of beach rock samples were analyzed using EDXRF.The samples were collected from three locations of Andaman Island.The Al,Ca,K,Fe,Ti,Si,V,Co,Cu,Ba,Zn,Pb,Cd and Mn contents were determined.The geochemical behavior of elements in the region is discussed.The elemental contents of beach rock samples from Andaman Island are much below the values of both earth crust and that of Tamilnadu region.However,content of the biogenic element Ca was the highest of all elements.This is due to the typical beach rock formation.
文摘Beach rocks samples were collected from South East Coast of Tamilnadu, India. The mineralogical composition was determined using FT-IR and XRD. The natural radioactive measurements to detect radioactive elements were determined by gamma ray spectrometer. The multi-element analyses were carried out by INAA (Instrumental neutron activation analysis), with the standard Estuarine Sediment as reference material. The geochemical behavior of elements in the region is discussed. The occurrence of the radioactive and non-radioactive elements is discussed for their geological significance. The results were used to assess environmental toxicity of heavy metals and radiation hazard in the study area.
文摘Element profiles of some beach rock samples collected from South East Coast of Tamilnadu, India have been determined using single comparator method of INAA. The geo-chemical behavior of the elements in the region is discussed. The irradiations were done at thermal neutron flux of ~ 1011 cm-2·s-1 at 20kW power using Kalpakkam Mini Reactor (KAMINI), IGCAR, Kalpakkam, Tamilnadu, India. Around 19 elements have been determined from 15 samples by high-resolution gamma spectrometry. The accuracy and precision were evaluated by assaying the irradiated Standard Reference Material (SRM 1646a Estuarine sediment) and were found to be in good agreement with certified values.
基金supported by the National Natural Science Foundation of China (Nos. 41672107, 41372119, 41440040)supports provided by the Marine Environmental Observation and Research Station at the Xisha Islands, the South China Sea Institute of Oceanology, CAS during the fieldwork
文摘Beach rock,which forms at the intertidal zone,is a natural barrier to protect beach and island from wave erosion. The formation mechanism of beach rocks is significant in the study of surface carbonate diagenesis and protection of island. Beach rocks in Qilian Islets and Cays were formed about 500–700 a BP,neither its composition nor sedimentary structure experienced intense post-reformation.Beach rocks in Qilian Islets and Cays are mainly composed of reef-building skeletal fragments and bioclasts without terrigenous sediments. This study focused on the types and morphologies of cements in beach rocks of Qilian Islets and Cays,and its cementation mechanisms and influencing factors. Biological activities,such as micritization caused by microbial activities and algae binding action,play an important role in the initial stage of bioclast transformation and promote the subsequent early marine and early meteoric cementation. Acicular aragonite induced by early marine cementation is well developed in beach rocks,especially in those samples from Medium Islet. Early meteoric cementation is not common as marine cementation,generally presenting granular and meniscus cements. The main factors affecting the formation and development of beach rocks in Qilian Islets and Cays include sediment source,hydrodynamic condition,climate,sea level change and anthropogenic impacts.
文摘The formation of beach rocks has a close relationship to storm deposits, denoted by beach and storm processes in association with depositional characteristics of the beach rocks found in Pui O and Lower Cheung Sha bays on the southern coast of Lantau Island, Hong Kong. Although not all beach rocks have an origin of storm deposits, it is certain that some of them with very coarse shells and shell fragments developing on sandy beaches originate from storm deposits. The cementation of beach rocks on a beach was affected directly by the texture and structure of the beach rocks and wave energy varying along the beach.
文摘Dune riocks are aeolian sands cemented ty calcium carbonate under subaerial conditions. They have been found in many of the coastal belts of Fujian, Guangdong and Hainan Provinces in South China. The grain composition of the dune rocks is mainly quartz sands and shell fragments. The quartz sands are medium and fine sized, relatively well sorted and positively skewed. Their surface texture formed in aeolian environments is characterized ty dishshaped depressions, meniscus depressions and V-shaped depressions with rounded edges. The most common bedding type of the rocks is larg (thickness>1.5m), steeply dipping (32--40°) with cross strata tolaner and convex upward). Mg and Sr contents are very low in the rock chemical composition which is classified into low Mg and low Sr category. The typical species of microfossils in the dune rocks are mainly freshwater ones and lack of typical saltwaer or semi-saltwater ones with incomplete assemblage of marine species. The cement minerals in the rocks are mainly low-Mg calcite and the common cement fabrics are meniscus cement and gravitational cement in response to impermanent water in vadose zones. Therefore, the dune rocks may be apparently distinguished from the beach rocks.
文摘The study investigates the potential of the serpulid tubeworm Ficopomatus sp.,sourced from Jesolo Lido(Venice,Italy),for CCS(Carbon Capture and Storage).Specimens were processed to extract bioactive compounds using a 50%polypropylene glycol-water solvent system.Extracts were analysed and purified using column gel filtration chromatography,with fractions identified by TLC(Thin Layer Chromatography)and further characterized for antioxidant and antibacterial activities.Antioxidant activity was detected via DPPH(2,2-Diphenyl-1-Picrylhydrazyl)spraying on TLC plates,while antibacterial activity was evaluated using the antibiogram paper disk diffusion method.Enzyme activity in the fractions was previously confirmed through a bromothymol blue test followed by spectrophotometric analysis.The primary goal was to explore the CCS potential,using an experimental module involving Arduino Uno embedded microprocessor for the CO_(2) measurement and to confirm the conversion into insoluble carbonates(storage).The most active fraction,identified as S1,showed significant CCS action,confirmed by microscopic observation of calcareous deposits on treated sponges.These findings suggest that Ficopomatus sp.can be used in CCS research highlighting its potential for biotechnological applications in mitigating climate change.The paper underscores the importance of marine organisms in CCS and offers insights into innovative strategies for environmental conservation and carbon management.
