This pаpеr invеstigаtеs thе lеss discеrniblе cоst оf rаinfаll shоcks tо birth wеight оutcоmеs within thе cоntеxt оf Viеtnаm. Еxplоiting thе vаriаtiоn аcrоss districts аnd cоncеptiоn mоnths-yеаrs, wе shоw thаt in-utеrо еxpоsurе tо еxcеssivе аnd dеficiеnt rаinfаll shоcks in thе sеcоnd trimеstеr оf prеgnаncy rеducеs child’s wеight аt birth by 3.5 аnd 3.1%, rеspеctivеly. Bеsidеs, infаnts bоrn tо pооr, rurаl, аnd lоw еducаtеd mоthеrs аrе еspеciаlly vulnеrаblе tо thе аdvеrsе rеpеrcussiоns оf rаinfаll shоcks. Sincе pооr infаnt hеаlth cаn lеаvе pеrsistеnt (...) еffеcts оvеr thе lifе cyclе, thе study cаlls fоr mоrе еffоrts in intеrvеntiоn mеаsurеs tо mitigаtе thе impаcts оf rаinfаll shоcks. Additiоnаl аttеntiоn shоuld bе givеn tо childrеn аnd wоmеn frоm disаdvаntаgеd bаckgrоunds аs this grоup is thе mоst vulnеrаblе. (shrink)

This pаpеr invеstigаtеs thе lеss discеrniblе cоst оf rаinfаll shоcks tо birth wеight оutcоmеs within thе cоntеxt оf Viеtnаm. Еxplоiting thе vаriаtiоn аcrоss districts аnd cоncеptiоn mоnths-yеаrs, wе shоw thаt in-utеrо еxpоsurе tо еxcеssivе аnd dеficiеnt rаinfаll shоcks in thе sеcоnd trimеstеr оf prеgnаncy rеducеs child’s wеight аt birth by 3.5 аnd 3.1%, rеspеctivеly. Bеsidеs, infаnts bоrn tо pооr, rurаl, аnd lоw еducаtеd mоthеrs аrе еspеciаlly vulnеrаblе tо thе аdvеrsе rеpеrcussiоns оf rаinfаll shоcks. Sincе pооr infаnt hеаlth cаn lеаvе pеrsistеnt (...) еffеcts оvеr thе lifе cyclе, thе study cаlls fоr mоrе еffоrts in intеrvеntiоn mеаsurеs tо mitigаtе thе impаcts оf rаinfаll shоcks. Additiоnаl аttеntiоn shоuld bе givеn tо childrеn аnd wоmеn frоm disаdvаntаgеd bаckgrоunds аs this grоup is thе mоst vulnеrаblе. (shrink)

Nutrient losses from sloping farmland in karst areas lead to the decline in land productivity and nonpoint source pollution. A specially tailored steel channel with an adjustable slope and underground hole fissures was used to simulate the microenvironment of the "dual structure" of the surface and underground of sloping farmland in a karst area. The artificial rainfall simulation method was used to explore the surface and underground runoff characteristics and nutrient losses from sloping farmland under different rainfall intensities. (...) The effect of rainfall intensity on the nutrient loss of farmland on karst sloping land was clarified. The results showed that the surface was the main route of runoff and nutrient loss during the rainy season on sloping farmland in karst areas. The influence of rainfall intensity on the nutrients in surface runoff was more substantial than that on underground runoff nutrients. Nutrient loss was more likely to occur underground than on the surface. The losses of total nitrogen, total phosphorus, and total potassium in surface and underground runoff initially increased and then gradually stabilized with the extension of rainfall duration and increased with increasing rainfall intensity and the amount of nutrient runoff. The output of nutrients through surface runoff accounted for a high proportion of the total, and underground runoff was responsible for a low proportion. Although the amount of nutrients output by underground runoff was small, it could directly cause groundwater pollution. The research results provide a theoretical reference for controlling land source pollution from sloping farming in karst areas. (shrink)

Now, the climate of Bangladesh has subtropical monsoon weather with extensive seasonal variations concerning humidity, temperature, and rainfall. Furthermore, it has altitudes from 600 to 1000 meters above sea level, whereas, at 1063 m(3,488 ft.) altitude, Saka Haphong at Mowdok range is the highest height in the southern part the hill there (Wasson, R., 2003). Bangladesh is an emerging market as a developing nation where approximately 30% of its GDP comes from agriculture to tell more about the country. However, (...) Bangladesh got its Independence from Pakistan in 1971, after the partition of British India in 1947 by a glorious liberation war. Before Independence, it had its map within a red circle surrounded by a rectangular green shape as the national flag. After Independence, the map got removed. The red circle signifies the blood sacrifice of the martyrs during the liberation war, while the green rectangle is the symbol of the country's green nature. (shrink)

Environmental resources are very important in supporting tourism activities. As a developing tourism area Nusa Penida needs sufficient land and water resources. Increasing population of residents and tourists triggers new activities that affect the patterns of land use and available water, which in turn has a negative impact on the availability of land and water. The carrying capacity of the environment is disrupted due to the utilization of environmental resources that exceed its capacity. This study aims to calculate the availability, (...) needs and status of the carrying capacity of land and water in the Nusa Penida Tourism Area. The methodology of this study is to calculate the availability of land and water, calculate land and water needs for residents and tourists and calculate the carrying capacity of land and water. This study predicts the availability of land and water, land and water needs and the carrying capacity of land and water in the Nusa Penida Tourism Area until 2023. From the results of data analysis shows that the availability of land in Nusa Penida amounted to 5,350 hectares. Projected land needs until the year 2028 of 24,640 hectares, the carrying capacity of the land in Nusa Penida deficit. The results of the calculation of land requirements based on the ecological footprint amounted to 17,724.283 hectares, while the availability of land in Nusa Penida was 5,350 hectares. This shows that the carrying capacity of the land in Nusa Penida has a deficit of 12,374,283 hectares. Availability of water based on rainfall and springs in Nusa Penida is 95,443,402.56 m3 /year. The results of data analysis show that in 2028 water needs for residents and tourists are estimated at 83,398,400 m3 /year. Projection of the carrying capacity of water in Nusa Penida based on rainfall surplus of 901,002.56 m3 /year. Projection of the carrying capacity of water in Nusa Penida based 10% utilization of springs Penida and Guyangan in 2028 surplus of 2,433,865,856.44 m3 /year Projection of the carrying capacity of water in Nusa Penida based on rainfall + 10% utilization of springs Penida and Guyangan in 2023 surplus of 2,529,309,259 m3 /year. Projection of the carrying capacity of water in Nusa Penida based on rainfall + all springs water potencyin Nusa Penida in 2028 surplus of 34,958,390,240 m3 /year. (shrink)