This work was done in order to characterize the water holding capacity and availability to plants in three soils of coastal tablelands in the state of Paraíba using tensiometry in areas cultivated with sugarcane. The water retention curves were determined for the Neossolo Quartzarenico, Latossolo Amarelo, Latossolo Coeso soils in the depths of 0 - 30cm and from 30 - 60 cm, by the Richards extractor method and by tensiometens in PVC columns in a greenhouse in the first phase and in a battery of field tensiometers in the second phase, in the tensions of 10, 20, 30, 40, 50 and 60 cm Hg. The water retention in the soils was significantly affected (p<0,01) as a function of the tensions (TS) applied. The same effect (p<0,01) was seen for the factor soil (S) and for the interaction (TS x S) both for the extractor and the greenhouse methods as well as for the field method. According to the study of the regression analysis, the mathematical model that showed the best adjustment was the decreasing quadratic. The values of moisture content found showed the most abrupt variations at the lowest tensions. The moisture content for the Neossolo Quartzarenico demonstrated under field conditions the importance of the structure for soils retaining more moisture in the tensions studied in relation to the laboratory and greenhouse methods. Even though the clay content were similar for the Latossolo Amarelo and the Latossolo. Coeso the greatest moisture retentions were observed in the Latossolo Coeso.