This data set is the runoff field data of Nanxiaohegou basin from 1954 to 1980. There are farmland, woodland, artificial pasture and standard plot for comparative observation. The main purpose is to reduce water and sediment benefits of soil and water conservation and the impact of terrain factors on Soil and water loss on slope. The area of runoff field is 30.5-1640 m2, and the observation elements include runoff, sediment, soil moisture, coverage and rainfall. The runoff and sediment are observed manually in the runoff bucket (pool). The soil moisture content was measured by manual sampling and drying method. The coverage was measured manually and visually.
| collect time | 1954/01/01 - 1980/12/31 |
|---|---|
| collect place | Nanxiaohegou watershed, houguanzhai Township, Xifeng District, Qingyang City, Gansu Province |
| altitude | 1050.0m - 1423.0m |
| data size | 1.5 MiB |
| Data time resolution | day |
| Coordinate system | WGS84 |
Artificial timing observation Instrument timing observation
(1) Runoff observation 1) Runoff pool: directly measure water after the end of runoff generation, and calculate the total runoff according to the water level volume curve. 2) Diversion bucket: the total amount of runoff can be calculated by the water distribution coefficient and the amount of water diversion. Total runoff (M3) = primary diversion bucket (M3) + secondary diversion bucket (M3) × number of primary diversion holes + +Runoff of n-stage diverter barrel (M3) × number of primary diversion holes × number of secondary diversion holes × Number of n-stage shunt holes (2) Sediment Observation 1) Runoff pool: observe immediately after the end of precipitation and runoff. The sludge and water in the collecting channel are swept into the runoff tank (bucket) and stirred evenly. Two to three columnar water samples (1000-3000ml in total) are taken, and 500ml water sample after mixing is taken as the standard sample. The sand content was determined by displacement method (Pycnometer method). 2) Diverter bucket: take samples separately, and the calculation is as follows: Total sediment (kg) = runoff of primary diversion bucket (M3) × sediment concentration (g / L) + runoff of secondary diversion bucket (M3) × sediment concentration (g / L) × number of primary diversion holes + +Runoff of n-stage diversion bucket (M3) × sediment concentration (g / L) × number of primary diversion holes × number of secondary diversion holes × Number of n-stage shunt holes
In the process of compilation and input of observation data, there are four levels of manual verification, including tabulation, primary calibration, recheck and audit, so as to ensure the data quality.
This work is licensed under
CC BY 4.0 (Creative Commons Attribution 4.0 International License).
| # | title | file size |
|---|---|---|
| 1 | 南小河沟径流场基本情况.zip | 150.2 KiB |
| 2 | 南小河沟径流场逐次径流泥沙测验成果表.zip | 72.9 KiB |
| 3 | (效)南小河沟径流场径流要素过程表.zip | 203.3 KiB |
| 4 | (效)南小河沟径流场逐日降水量表.zip | 94.5 KiB |
| 5 | (效)南小河沟径流场逐次径流泥沙测验成果表.zip | 584.3 KiB |
| 6 | (效)南小河沟径流场降水量摘录表.zip | 429.6 KiB |
1954 1955 1956 1957 1958 1959 1960 1961 1962 1963 1964 1965 1966 1967 1968 1969 1970 1971 1972 1973 1974 1975 1976 1977 1978 1979 1980
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©Copyright 2005-. Northwest Institute of Eco-Environment and Resources, CAS.
Donggang West Road 320, Lanzhou, Gansu, China (730000)

