Mm over the last 10 years, using a imply annual value of 941.08 mm plus a mean day-to-day value of two.56 mm [68]. In BLQ1 and BLQ2, annual precipitation ranged from 1324 mm to 2146 mm amongst 2010 and 2016, with a mean annual value of 1698 mm and also a imply day-to-day worth of four.65 mm. UCB-5307 Technical Information Average monthly flow reaches its maximum values within the months of July, August and September inside the four catchments. BLQ1 exhibited the 20(S)-Hydroxycholesterol Data Sheet highest flow values, followed by BLQ2, Q2 and Q3. Minimum average month-to-month flows are reached within the summer time months (January to March) for the four study catchments, especially within the months of February and March (Figure 2c). Surface, land cover and elevation characteristics are presented in Table 1. Q2 is covered by Nothofagus glauca (Hualo) because the dominant species, a native and winter deciduous species [68]. Q3 is often a mixed catchment covered by Pinus radiata planted in 2001 (62 ) and native forest with N. glauca because the most important species (34 ). BLQ1 and BLQ2 are covered by Eucalyptus nitens plantations with an initial stock density of 1666 trees ha-1 ; no forest management was performed in these catchments [3]. In Q2 and Q3, soils have originated from metamorphic rocks [3,68] using a topography of hills and ridges, with variable and complicated slopes. The soil is shallow, with depths involving 0 and 100 cm and organic matter amongst three and 4 on the surface [69], and is composed of silt, clay and sand inside the order of 36, 40 and 24 , respectively [68]. The soil has rock fragments, and the subsoil rock is dominated by deep seams of partially weathered material [68]. Soils of BLQ1 and BLQ2 have their origin within the group of metamorphic soils which have been formed from material generating shales, sandstones, phyllites and schists [69]. Normally, these soils have clay textures, low water infiltration and occupy positions that vary from abrupt hills and mountain ranges with variable and complexWater 2021, 13,5 ofWater 2021, 13, x FOR PEER Critique slopes.five of 30 They present a physiography of mountains dissected by deep ravines, mountainous topography, very good external drainage, moderate internal drainage and parent material composed of shales [69].Water 2021, 13, x FOR PEER REVIEW6 ofFigure 1. Geographical place of your catchments beneath study in south-central Chile. Figure 1. Geographical location with the catchments under study in south-central Chile.Concerning the climatological characteristics in the catchment, dry months are from November to March, and rainy months are from Could to August. Each of the catchments have a similar intra-annual distribution of precipitation and temperature (Figure 2a,b). Annual precipitation in Q2 and Q3 varied in between 727 and 1342 mm more than the last 10 years, having a imply annual value of 941.08 mm as well as a mean daily worth of two.56 mm [68]. In BLQ1 and BLQ2, annual precipitation ranged from 1324 mm to 2146 mm involving 2010 and 2016, using a imply annual worth of 1698 mm plus a imply every day worth of four.65 mm. Typical month-to-month flow reaches its maximum values inside the months of July, August and September inside the four catchments. BLQ1 exhibited the highest flow values, followed by BLQ2, Q2 and Q3. Minimum typical monthly flows are reached in the summer season months (January to March) for the 4 study catchments, specifically inside the months of February and March (Figure 2c). Surface, land cover and elevation qualities are presented in Table 1.Table 1. Vegetation cover and geomorphological data of surface (ha), exposure ( and slope ( in the catchments. Catchmen.