FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2883205712> ?p ?o ?g. }

• W2883205712 endingPage "177" @default.
• W2883205712 startingPage "163" @default.
• W2883205712 abstract "Imperata grassland soils are widely perceived as having poor physical and chemical properties that render them unproductive and prone to erosion. They are therefore increasingly targeted for reforestation across the tropics. To better understand how reforestation and forest growth affect soil hydrological processes we compared the soil physical characteristics for an Imperata grassland and a 23-year-old ‘reforest’ on Leyte Island, the Philippines. Saturated hydraulic conductivity (Ksat) was determined in the field (Amoozemeter, 20–90 cm depth) and the laboratory (small-core permeametry). Core-based values of Ksat were (much) lower than field-based values, suggesting macropores were not sampled adequately with the small cores. Ksat decreased exponentially with depth in both land-cover types, with a median field-measured Ksat of the grassland of 2.1 mm h−1 at the surface and 2.9 mm h−1 at 20–40 cm depth, declining to ≤1 mm h−1 below 60 cm. Corresponding values for the reforest were 59 (at 20 cm), 37 (at 40 cm) and 7.3 mm h−1 (at 60–100 cm depth). Reforest Ksat-values down to 60 cm depth were significantly higher than corresponding values in the grassland, but the difference disappeared at 90 cm depth. Organic carbon content in the top 40 cm of soil was slightly higher in the reforest than the grassland. Bulk density was higher and porosity marginally lower in the grassland than the reforest at all depths considered. The median five-min rainfall intensity (June 2013–May 2014) was 3.2 mm h−1, suggesting that >50% of the rainfall might generate Hortonian overland flow in the grassland. Overland flow is unlikely in the reforest where lateral flow is likely to be generated around 60 cm depth for ~30% of rain-time, versus 2–3% between 20 and 60 cm. Within the limitations of the space-for-time substitution approach, these results suggest that 23 years of forest development at Manobo had a positive effect on hillslope hydrological functioning." @default.
• W2883205712 created "2018-08-03" @default.
• W2883205712 creator A5022645100 @default.
• W2883205712 creator A5023484674 @default.
• W2883205712 creator A5030268268 @default.
• W2883205712 creator A5032388817 @default.
• W2883205712 creator A5051339983 @default.
• W2883205712 creator A5084230647 @default.
• W2883205712 date "2019-01-01" @default.
• W2883205712 modified "2023-09-27" @default.
• W2883205712 title "Soil physical characteristics of a degraded tropical grassland and a ‘reforest’: Implications for runoff generation" @default.
• W2883205712 cites W138814786 @default.
• W2883205712 cites W1569082154 @default.
• W2883205712 cites W1684875526 @default.
• W2883205712 cites W1930412689 @default.
• W2883205712 cites W1943133802 @default.
• W2883205712 cites W1967571818 @default.
• W2883205712 cites W1968466506 @default.
• W2883205712 cites W1970691485 @default.
• W2883205712 cites W1974154763 @default.
• W2883205712 cites W1974978848 @default.
• W2883205712 cites W1977081610 @default.
• W2883205712 cites W1982606854 @default.
• W2883205712 cites W1982633889 @default.
• W2883205712 cites W1990004181 @default.
• W2883205712 cites W1990736187 @default.
• W2883205712 cites W1991570070 @default.
• W2883205712 cites W2004284115 @default.
• W2883205712 cites W2005523086 @default.
• W2883205712 cites W2009501387 @default.
• W2883205712 cites W2011642679 @default.
• W2883205712 cites W2013820090 @default.
• W2883205712 cites W2017458046 @default.
• W2883205712 cites W2021166199 @default.
• W2883205712 cites W2032610955 @default.
• W2883205712 cites W2039826136 @default.
• W2883205712 cites W2040173543 @default.
• W2883205712 cites W2041878347 @default.
• W2883205712 cites W2042134029 @default.
• W2883205712 cites W2046502966 @default.
• W2883205712 cites W2049496607 @default.
• W2883205712 cites W2052996421 @default.
• W2883205712 cites W2059023083 @default.
• W2883205712 cites W2067123747 @default.
• W2883205712 cites W2067888477 @default.
• W2883205712 cites W2068144866 @default.
• W2883205712 cites W2071908967 @default.
• W2883205712 cites W2076285931 @default.
• W2883205712 cites W2089720789 @default.
• W2883205712 cites W2091998201 @default.
• W2883205712 cites W2094103414 @default.
• W2883205712 cites W2094214979 @default.
• W2883205712 cites W2095898584 @default.
• W2883205712 cites W2096345554 @default.
• W2883205712 cites W2099460409 @default.
• W2883205712 cites W2100413889 @default.
• W2883205712 cites W2102293625 @default.
• W2883205712 cites W2105111145 @default.
• W2883205712 cites W2125065961 @default.
• W2883205712 cites W2127514772 @default.
• W2883205712 cites W2129972701 @default.
• W2883205712 cites W2132185647 @default.
• W2883205712 cites W2133695883 @default.
• W2883205712 cites W2139362435 @default.
• W2883205712 cites W2140302389 @default.
• W2883205712 cites W2147930996 @default.
• W2883205712 cites W2148679320 @default.
• W2883205712 cites W2148800137 @default.
• W2883205712 cites W2149950587 @default.
• W2883205712 cites W2151149235 @default.
• W2883205712 cites W2156216463 @default.
• W2883205712 cites W2166341880 @default.
• W2883205712 cites W2167194281 @default.
• W2883205712 cites W2167422772 @default.
• W2883205712 cites W2174069807 @default.
• W2883205712 cites W2277236915 @default.
• W2883205712 cites W2295283661 @default.
• W2883205712 cites W2319481566 @default.
• W2883205712 cites W2328507442 @default.
• W2883205712 cites W2335717164 @default.
• W2883205712 cites W2339760897 @default.
• W2883205712 cites W239403212 @default.
• W2883205712 cites W2402247296 @default.
• W2883205712 cites W2582235644 @default.
• W2883205712 cites W2775145615 @default.
• W2883205712 doi "https://doi.org/10.1016/j.geoderma.2018.07.022" @default.
• W2883205712 hasPublicationYear "2019" @default.
• W2883205712 type Work @default.
• W2883205712 sameAs 2883205712 @default.
• W2883205712 citedByCount "35" @default.
• W2883205712 countsByYear W28832057122018 @default.
• W2883205712 countsByYear W28832057122019 @default.
• W2883205712 countsByYear W28832057122020 @default.
• W2883205712 countsByYear W28832057122021 @default.
• W2883205712 countsByYear W28832057122022 @default.
• W2883205712 countsByYear W28832057122023 @default.
• W2883205712 crossrefType "journal-article" @default.
• W2883205712 hasAuthorship W2883205712A5022645100 @default.

• next