Shoreline erosion has been a pernicious problem facing many countries around the world.It causes the degradation and vulnerability of coastal eco-environments,and imposes considerable pressures upon coastal economic,s...Shoreline erosion has been a pernicious problem facing many countries around the world.It causes the degradation and vulnerability of coastal eco-environments,and imposes considerable pressures upon coastal economic,social developments in the context of climate change and sea-level rising.The muddy coast of the abandoned Yellow River delta at Binhai,Jiangsu Province,China has experienced chronic erosion since 1855 when the Yellow River avulsed to north China.A variety of hard structures,that is,seawall,groin,jetty,breakwater,and so forth were emplaced and reinforced to withstand the shoreline retreat and concomitant beach loss.These engineering solutions have been proved unsuccessful or ineffective in their objectives.An overview is presented on the multi-decadal defense endeavors with technical lessons and management implications learnt.A SHIAA(site-specific,holistic,integrative,adaptive,affordable)tenet is put forward to achieve the sustainability in a coastal erosion mitigation scheme.The merit and limitation of nature-based solutions(NBS)applied in coastal protection is further discussed.展开更多
In addressing problematic soils,geotechnical engineers employ two key strategies:compatibility and improvement.This study focuses on soft and CL deltaic sediments,and seeks to enhance cementation by investigating micr...In addressing problematic soils,geotechnical engineers employ two key strategies:compatibility and improvement.This study focuses on soft and CL deltaic sediments,and seeks to enhance cementation by investigating microbially-induced calcium carbonate precipitation(MICP).Sporosarcina pasteurii bacteria,together with a cementation solution(urea and calcium-containing salt),were electrokinetically injected into deltaic clay soil from the Telar River in Iran.The initial samples,with a dry unit weight(γ_(d))of 12.75 kN/m^(3),underwent injections in two modes:simultaneous injection of the bacterial and cementation solutions and individual injection in a sequential order.Unconfined compression strength tests and laboratory vane shear tests were conducted to assess changes in soil strength parameters,while a consolidation test was performed to investigate alterations in soil settlement parameters.A comparative analysis with an electroosmosis control sample revealed a remarkable increase in compressive strength and undrained shear strength for MICP bio-electrokinetic improvement.Moreover,the consolidation test demonstrated that the compression index(C_(c))and recompression index(C_(r))exhibited a more pronounced decline in the simultaneous injection than individual injection.This highlights the dual impact of the bio-electrokinetic method,namely the enhancement of shear strength and the mitigation of settlement in deltaic clay soil.The calcium carbonate content was measured for the samples,and the results indicated a higher degree of participation for the samples subjected to simultaneous injection.Microstructure analyses were conducted on samples,and calcite and vaterite were observed in biocemented samples.展开更多
There are large deltaic systems in the Triassic Yanchang Formation in the northern Shaanxi area of the Ordos Basin, and developed two sets of good source-reservoir-caprock assemblages and many sets of oil-bearing beds...There are large deltaic systems in the Triassic Yanchang Formation in the northern Shaanxi area of the Ordos Basin, and developed two sets of good source-reservoir-caprock assemblages and many sets of oil-bearing beds. Exploration experience demonstrates that the formation and distribution of the reservoir were controlled by the generative depression of the Yanchang Formation, and deltaic reservoir sand body is the material basis for large-scale oilfields. In addition, secondary laumontite in a low permeable area was dissolved and then a high permeable area was formed. The updip lithologic variety of reservoir sand bodies is favorable to the formation of subtle lithologic traps, and the deltaic reservoirs are characterized by large multi-beds of oil-generation and abundant hydrocarbon resources. In this paper, the petroleum geologic settings of the studied area are analyzed, and the accumulation characteristics and exploration methods of lithologic reservoirs are summarized. It is of theoretical significance for the study of the exploration theories of lithologic reservoirs, and also expedites the exploration steps of deltaic reservoirs in the northern Shaanxi area.展开更多
A macro-tidal tropical estuary with high fluvial discharge is characterized by both fragility and remarkable dynamism.This study utilizes the Salween River Delta(SRD)as a case example to examine the interplay between ...A macro-tidal tropical estuary with high fluvial discharge is characterized by both fragility and remarkable dynamism.This study utilizes the Salween River Delta(SRD)as a case example to examine the interplay between morphology and vegetation under similar tidal conditions.Our analysis of correlations and inferences revealed several significant trends in the SRD:(1)an overall expansion of land area and intertidal vegetation,with the most pronounced changes occurring in the eastern sector;(2)the predominance of river discharge influencing the southwestern and northern sectors,contrasted with the primary impact of storm surges in the eastern sector;and(3)three distinct causal relationships among estuarine morphology,vegetation,storm surges,and river discharge:a direct model where river discharge shapes estuarine morphology,a progressive model in which river discharge affects vegetation distribution,subsequently influencing estuarine morphology,and a hybrid model where storm surges directly impact vegetation and indirectly modify its distribution through changes in estuarine morphology.The stability of sediment supply and the role of intertidal vegetation are crucial for the continuous seaward advance,providing a vital foundation for the protection and development of estuarine deltas.展开更多
The Late Triassic Mungaroo Formation of the Exmouth Plateau was investigated through an integrated,stratigraphically and geographically extensive study to characterize its source rock potential and depositional contro...The Late Triassic Mungaroo Formation of the Exmouth Plateau was investigated through an integrated,stratigraphically and geographically extensive study to characterize its source rock potential and depositional controls.Geochemical,petrographic,and palynological analyses reveal highly variable organic richness across the formation,with total organic carbon(TOC) content values ranging from very low in sand-dominated intervals to notably high in coal-bearing mudstones.The Mungaroo Formation exhibits diverse organic composition,with TOC content ranging from 0.63 % to 54.18 %,demonstrating that while certain intervals contain significant organic richness,others are notably lean in organic content.Petrographic analyses reveal the presence of dinoflagellates,liptodetrinite,sporinite,and cutinite,suggesting transitional settings with varying marine influence.Thermal maturity assessments indicate a range of maturity levels,with vitrinite reflectance(Ro) values ranging from 0.45 % to 1.39 %,reflecting thermal maturity of immature to post-mature stage.Rock-Eval pyrolysis parameters support these observations,highlighting varying stages of hydrocarbon generation.Biomarker characteristics further confirm the mixed organic origin and complex paleo-depositional environments within the Mungaroo Formation.The presence of both marine and terrigenous biomarkers underscores the depositional history of the region,with Pristane/Phytane ratios(Pr/Ph) indicating oxidizing environments typically associated with terrigenous plants' input.Palynological data indicates strong terrigenous influence within both the wells Mercury-1 and Jupiter-1,characterized by proximal delta-plain environments.展开更多
The geological background of the fluvial and lacustrine depository system in the large mid-shallow layered depressed lake in the Songliao Basin has been proven to have the geological conditions for the formation of li...The geological background of the fluvial and lacustrine depository system in the large mid-shallow layered depressed lake in the Songliao Basin has been proven to have the geological conditions for the formation of lithologic reservoirs over a large area. Because the rise and fall of the base level caused considerable differences in the space at different periods, the types of sand bodies varied in different geologic periods; but at the same time, because of the differences in burial depths and the relative differences in positions of the siltstones and source rocks, the formation conditions and distributive regularities for oil-bearing groups of subtle reservoirs also vary accordingly. In view of the reality of the thinly-interbedded lithologic reservoir in the deltaic frontal facies belt, we have conducted a series of research to study the thinly-interbedded subtle reservoirs with the help of high resolution sequence stratigraphy, pattern recognition and the geophysical recognition and prediction techniques for thinly-interbedded subtle reservoirs, thus achieving a better effect and optimizing several exploration target areas, each of which has an oil reserve of about 100 million tons. This has shed light on further exploration of new subtle reservoirs.展开更多
基金National Natural Science Foundation of China,Grant/Award Number:12202503。
文摘Shoreline erosion has been a pernicious problem facing many countries around the world.It causes the degradation and vulnerability of coastal eco-environments,and imposes considerable pressures upon coastal economic,social developments in the context of climate change and sea-level rising.The muddy coast of the abandoned Yellow River delta at Binhai,Jiangsu Province,China has experienced chronic erosion since 1855 when the Yellow River avulsed to north China.A variety of hard structures,that is,seawall,groin,jetty,breakwater,and so forth were emplaced and reinforced to withstand the shoreline retreat and concomitant beach loss.These engineering solutions have been proved unsuccessful or ineffective in their objectives.An overview is presented on the multi-decadal defense endeavors with technical lessons and management implications learnt.A SHIAA(site-specific,holistic,integrative,adaptive,affordable)tenet is put forward to achieve the sustainability in a coastal erosion mitigation scheme.The merit and limitation of nature-based solutions(NBS)applied in coastal protection is further discussed.
文摘In addressing problematic soils,geotechnical engineers employ two key strategies:compatibility and improvement.This study focuses on soft and CL deltaic sediments,and seeks to enhance cementation by investigating microbially-induced calcium carbonate precipitation(MICP).Sporosarcina pasteurii bacteria,together with a cementation solution(urea and calcium-containing salt),were electrokinetically injected into deltaic clay soil from the Telar River in Iran.The initial samples,with a dry unit weight(γ_(d))of 12.75 kN/m^(3),underwent injections in two modes:simultaneous injection of the bacterial and cementation solutions and individual injection in a sequential order.Unconfined compression strength tests and laboratory vane shear tests were conducted to assess changes in soil strength parameters,while a consolidation test was performed to investigate alterations in soil settlement parameters.A comparative analysis with an electroosmosis control sample revealed a remarkable increase in compressive strength and undrained shear strength for MICP bio-electrokinetic improvement.Moreover,the consolidation test demonstrated that the compression index(C_(c))and recompression index(C_(r))exhibited a more pronounced decline in the simultaneous injection than individual injection.This highlights the dual impact of the bio-electrokinetic method,namely the enhancement of shear strength and the mitigation of settlement in deltaic clay soil.The calcium carbonate content was measured for the samples,and the results indicated a higher degree of participation for the samples subjected to simultaneous injection.Microstructure analyses were conducted on samples,and calcite and vaterite were observed in biocemented samples.
文摘There are large deltaic systems in the Triassic Yanchang Formation in the northern Shaanxi area of the Ordos Basin, and developed two sets of good source-reservoir-caprock assemblages and many sets of oil-bearing beds. Exploration experience demonstrates that the formation and distribution of the reservoir were controlled by the generative depression of the Yanchang Formation, and deltaic reservoir sand body is the material basis for large-scale oilfields. In addition, secondary laumontite in a low permeable area was dissolved and then a high permeable area was formed. The updip lithologic variety of reservoir sand bodies is favorable to the formation of subtle lithologic traps, and the deltaic reservoirs are characterized by large multi-beds of oil-generation and abundant hydrocarbon resources. In this paper, the petroleum geologic settings of the studied area are analyzed, and the accumulation characteristics and exploration methods of lithologic reservoirs are summarized. It is of theoretical significance for the study of the exploration theories of lithologic reservoirs, and also expedites the exploration steps of deltaic reservoirs in the northern Shaanxi area.
基金National Natural Science Foundation of China,No.41906148,No.42271086Rejuvenating Yunnan Talents Support Plan Young Talent Program,No.XDYC-QNRC-2023-0322。
文摘A macro-tidal tropical estuary with high fluvial discharge is characterized by both fragility and remarkable dynamism.This study utilizes the Salween River Delta(SRD)as a case example to examine the interplay between morphology and vegetation under similar tidal conditions.Our analysis of correlations and inferences revealed several significant trends in the SRD:(1)an overall expansion of land area and intertidal vegetation,with the most pronounced changes occurring in the eastern sector;(2)the predominance of river discharge influencing the southwestern and northern sectors,contrasted with the primary impact of storm surges in the eastern sector;and(3)three distinct causal relationships among estuarine morphology,vegetation,storm surges,and river discharge:a direct model where river discharge shapes estuarine morphology,a progressive model in which river discharge affects vegetation distribution,subsequently influencing estuarine morphology,and a hybrid model where storm surges directly impact vegetation and indirectly modify its distribution through changes in estuarine morphology.The stability of sediment supply and the role of intertidal vegetation are crucial for the continuous seaward advance,providing a vital foundation for the protection and development of estuarine deltas.
文摘The Late Triassic Mungaroo Formation of the Exmouth Plateau was investigated through an integrated,stratigraphically and geographically extensive study to characterize its source rock potential and depositional controls.Geochemical,petrographic,and palynological analyses reveal highly variable organic richness across the formation,with total organic carbon(TOC) content values ranging from very low in sand-dominated intervals to notably high in coal-bearing mudstones.The Mungaroo Formation exhibits diverse organic composition,with TOC content ranging from 0.63 % to 54.18 %,demonstrating that while certain intervals contain significant organic richness,others are notably lean in organic content.Petrographic analyses reveal the presence of dinoflagellates,liptodetrinite,sporinite,and cutinite,suggesting transitional settings with varying marine influence.Thermal maturity assessments indicate a range of maturity levels,with vitrinite reflectance(Ro) values ranging from 0.45 % to 1.39 %,reflecting thermal maturity of immature to post-mature stage.Rock-Eval pyrolysis parameters support these observations,highlighting varying stages of hydrocarbon generation.Biomarker characteristics further confirm the mixed organic origin and complex paleo-depositional environments within the Mungaroo Formation.The presence of both marine and terrigenous biomarkers underscores the depositional history of the region,with Pristane/Phytane ratios(Pr/Ph) indicating oxidizing environments typically associated with terrigenous plants' input.Palynological data indicates strong terrigenous influence within both the wells Mercury-1 and Jupiter-1,characterized by proximal delta-plain environments.
文摘The geological background of the fluvial and lacustrine depository system in the large mid-shallow layered depressed lake in the Songliao Basin has been proven to have the geological conditions for the formation of lithologic reservoirs over a large area. Because the rise and fall of the base level caused considerable differences in the space at different periods, the types of sand bodies varied in different geologic periods; but at the same time, because of the differences in burial depths and the relative differences in positions of the siltstones and source rocks, the formation conditions and distributive regularities for oil-bearing groups of subtle reservoirs also vary accordingly. In view of the reality of the thinly-interbedded lithologic reservoir in the deltaic frontal facies belt, we have conducted a series of research to study the thinly-interbedded subtle reservoirs with the help of high resolution sequence stratigraphy, pattern recognition and the geophysical recognition and prediction techniques for thinly-interbedded subtle reservoirs, thus achieving a better effect and optimizing several exploration target areas, each of which has an oil reserve of about 100 million tons. This has shed light on further exploration of new subtle reservoirs.
