Carbon-14 transfers between two compartments of the environment are generally evaluated based on the assumption that the isotopic ratio between the radioactive carbon and the stable carbon (considered to be C and that equilibrium between the two compartments is achieved.Under this assumption, the impact on the environment and populations can only be evaluated for environmental releases and concentrations that are constant over time, generally by using average annual values.Early political consolidations took place under the Maurya and Gupta empires; the later peninsular Middle Kingdoms influenced cultures as far as southeast Asia.In the medieval era, Judaism, Zoroastrianism, Christianity, and Islam arrived, and Sikhism emerged, all adding to the region's diverse culture.is incorporated in the organic material, forming its carbon skeleton. The radioactive half-life is higher than a year only for carbon-14, its maximum value for the other isotopes being around 20 minutes. Production fluctuates due to variation in cosmic ray intensity.
In the Indian Ocean, India is in the vicinity of Sri Lanka and the Maldives.
Health conditions that may lead to CHF include: coronary artery disease, hypertension (high blood pressure), or arrhythmias.
Symptoms of heart failure include shortness of breath and abnormal fluid retention, which usually results in swelling in the feet and legs.
Congestive heart failure (CHF), or heart failure, is a condition in which the heart is unable to adequately pump blood throughout the body and/or unable to prevent blood from accumulating, or "backing up," into the lungs.
In most cases, CHF is a process that occurs over time, when an underlying condition damages the heart or makes it work too hard, weakening the organ.