Sentence examples for segments of order from inspiring English sources

The mean stream lengths were calculated using the formula of total stream length of order divided by total number of stream segments of order.

Mean stream length Lsm = Lu/Nu, where, Lu = total stream length of order "u", Nu = total no. of stream segments of order u Strahler (1964)  4.

Bifurcation ratio Rb = Nu/Nu + 1, Nu = total number of stream segments of order "u", Nu + 1 = number pf stream segments of the next higher order Schumn (1956)  6.

The mean stream length (Lsm) is computed by dividing the total stream length of order "Lu" by the number of stream segments of order "Nu" (Srinivasa et al. 2004).

Horton (1945) states that the length ratio is the ratio of the mean (L ur) of segments of order (S o) to mean length of segments of the next lower order (L u−1), which tends to be constant throughout the successive orders of a basin.

According to Strahler (1964) method, two first-order streams join and form the channel segment of order 2.

Where two 2-order stream join, the channel segment of order 3 formed, likewise stream orders are increasing.

Stream order-wise mean length in each watershed was obtained by dividing the total length of streams of a particular order by the total number of stream segments of the order.

Number of streams is also described as total counts of stream segments of different order separately and is inversely proportional to the stream order.

According to the Horton's laws of stream number explained that the number of stream segments of each order form an inverse geometric sequence with plotted against order, which means that the number of streams usually decreases in geometric progression as the stream order increases (Rao et al. 2010; Sreedevi et al. 2013; Pande and Moharir 2015).

According to Schumn (1956), the term bifurcation ratio (Rb) may be defined as the ratio of the number of the stream segments of given order to the number of segments of the next higher orders.