At the beginning of 1990 a discussion started among physicists at Bell Lab, Milano University and INFN on the possibility to design a detector to measure the solar neutrinos at low energy, say below ∼ 2 MeV: the goal at the beginning was, first of all, the measurement of the neutrino flux from 7 Be at 0.867 MeV.At that time solar neutrinos were studied by the radiochemical experiments, such as Homestake, GALLEX and Sage. At the same time the Cherenkov detectors were either running or in preparation.The radiochemical experiments were able to measure only an integrated neutrino flux from a lower threshold: 0.814 MeV for Homestake and 0.233 MeV for GALLEX, but not the single fluxes produced by the various reactions expected to be the source of the Sun shining. The real time Cherenkov experiments faced a high background due to the decay products of the natural radioactive contaminants from the construction materials and the environment, which reach an upper energy limit of ∼ 3 MeV (Tallium nuclides); energy thresholds at relatively high energy as ∼ 7 MeV or ∼ 5 MeV have been the solution adopted by these experiments. Only later some attempts have been done to lower the thresholds, which, however, did not allow to measure flows other than the high energy tail of the 8 B neutrinos.For the solar neutrinos, the lower is the neutrino energy, the higher is the neutrino flux. The pp reaction produces by far the highest rate, while the direct daughter reaction involving 7 Be is the second solar neutrino producer. The 8 B tile measured by the Cherenkov experiments contributes a ∼ 0.01% to the total solar neutrinos.The new detector has been conceived to have high resolution and an unprecedented radio-purity. These constraints suggested to choose as detecting material a liquid scintillator and to develop an R&D, which lasted four years, to develop 1402002-1 Int. J. Mod. Phys. A 2014.29. Downloaded from www.worldscientific.com by UNIVERSITY OF PITTSBURGH on 06/25/14. For personal use only. 1402002-2 Int. J. Mod. Phys. A 2014.29. Downloaded from www.worldscientific.com by UNIVERSITY OF PITTSBURGH on 06/25/14. For personal use only.