Variability in leaf wettability and surface water retention of main species in semiarid Loess Plateau of China

Ecohydrology ◽  
2018 ◽  
Vol 11 (8) ◽  
pp. e2021 ◽  
Author(s):  
Peifeng Xiong ◽  
Zhifei Chen ◽  
Zhao Jia ◽  
Zhi Wang ◽  
Jairo A. Palta ◽  
...  
Keyword(s):  
Surface Water ◽  
Loess Plateau ◽  
Water Retention ◽  
Main Species ◽  
Leaf Wettability

scholarly journals Effect of Nano-Carbon on Water Holding Capacity in a Sandy Soil of the Loess Plateau

2017 ◽  
Vol 21 (4) ◽  
pp. 189-195 ◽  
Author(s):  
Beibei Zhou ◽  
Xiaopeng Chen
Keyword(s):  
Water Content ◽  
Soil Water ◽  
Loess Plateau ◽  
Sandy Soil ◽  
Water Retention ◽  
Soil Mixture ◽  
Cumulative Infiltration ◽  
Nano Carbon ◽  
Water Contents ◽  
Soil Water Contents

The poor water retention capacity of sandy soils commonly aggregate soil erosion and ecological environment on the Chinese Loess Plateau. Due to its strong capacity for absorption and large specific surface area, the use of nanocarbon made of coconut shell as a soil amendment that could improve water retention was investigated. Soil column experiments were conducted in which a layer of nanocarbon mixed well with the soil was formed at a depth of 20 cm below the soil surface. Four different nanocarbon contents by weight (0%, 0.1%, 0.5%, and 1%) and five thicknesses of the nanocarbon- soil mixture layer ranging from 1 to 5 cm were considered. Cumulative infiltration and soil water content distributions were determined when water was added to soil columns. Soil Water Characteristic Curves (SWCC) were obtained using the centrifuge method. The principal results showed that the infiltration rate and cumulative infiltration increased with the increases of nanocarbon contents, to the thicknesses of the nano carbon-soil mixture layer. Soil water contents that below the soil-nano carbon layer decreased sharply. Both the Brooks-Corey and van Genuchten models could describe well the SWCC of the disturbed sandy soil with various nano carbon contents. Both the saturated water content (θs), residual water content (θr) and empirical parameter (α) increased with increasing nano carbon content, while the pore-size distribution parameter (n) decreased. The available soil water contents were efficiently increased with the increase in nanocarbon contents.

Surface water storage characteristics of main herbaceous species in semiarid Loess Plateau of China

Ecohydrology ◽  
2019 ◽  
Vol 12 (8) ◽  
Author(s):  
Peifeng Xiong ◽  
Zhifei Chen ◽  
Quan Yang ◽  
Junjie Zhou ◽  
He Zhang ◽  
...  
Keyword(s):  
Surface Water ◽  
Loess Plateau ◽  
Water Storage ◽  
Herbaceous Species ◽  
Storage Characteristics ◽  
Surface Water Storage

scholarly journals Nitrogen surface water retention in the Baltic Sea drainage basin

2014 ◽  
Vol 11 (9) ◽  
pp. 10829-10858 ◽  
Author(s):  
P. Stålnacke ◽  
A. Pengerud ◽  
A. Vassiljev ◽  
E. Smedberg ◽  
C.-M. Mörth ◽  
...  
Keyword(s):  
Surface Water ◽  
Baltic Sea ◽  
Water Retention ◽  
Action Plan ◽  
River Basins ◽  
Lake Area ◽  
The Baltic Sea ◽  
Total N ◽  
N Retention ◽  
The Baltic

Abstract. In this paper, we estimate the surface water retention of nitrogen (N) in all the 117 drainage basins to the Baltic Sea with the use of a statistical model (MESAW) for source apportionment of riverine loads of pollutants. Our results show that the MESAW model was able to estimate the N load at the river mouth of 88 Baltic Sea rivers, for which we had observed data, with a sufficient degree of precision and accuracy. The estimated retention parameters were also statistically significant. Our results show that around 380 000 t of N are annually retained in surface waters draining to the Baltic Sea. The total annual riverine load from the 117 basins to the Baltic Sea was estimated to 570 000 t of N, giving a total surface water N retention of around 40%. In terms of absolute retention values, three major river basins account for 50% of the total retention in the 117 basins; i.e. around 104 000 t of N is retained in Neva, 55 000 t in Vistula and 32 000 t in Oder. The largest retention was found in river basins with a high percentage of lakes as indicated by a strong relationship between N retention (%) and share of lake area in the river drainage areas. For example in Göta älv, we estimated a total N retention of 72%, whereof 67% of the retention occurred in the lakes of that drainage area (Lake Vänern primarily). The obtained results will hopefully enable the Helsinki Commission (HELCOM) to refine the nutrient load targets in the Baltic Sea Action Plan (BSAP), as well as to better identify cost-efficient measures to reduce nutrient loadings to the Baltic Sea.

Dynamics and ecological strategies of aerial seed bank of main species in the hill-gully Loess Plateau

2015 ◽  
Vol 35 (5) ◽  
Author(s):  
王东丽 WANG Dongli ◽  
焦菊英 JIAO Juying ◽  
陈宇 CHEN Yu ◽  
寇萌 KOU Meng ◽  
尹秋龙 YIN Qiulong ◽  
...  
Keyword(s):  
Loess Plateau ◽  
Seed Bank ◽  
Ecological Strategies ◽  
Main Species ◽  
The Hill

scholarly journals Nitrogen surface water retention in the Baltic Sea drainage basin

2015 ◽  
Vol 19 (2) ◽  
pp. 981-996 ◽  
Author(s):  
P. Stålnacke ◽  
A. Pengerud ◽  
A. Vassiljev ◽  
E. Smedberg ◽  
C.-M. Mörth ◽  
...  
Keyword(s):  
Surface Water ◽  
Baltic Sea ◽  
Water Retention ◽  
Action Plan ◽  
River Basins ◽  
Lake Area ◽  
The Baltic Sea ◽  
Total N ◽  
N Retention ◽  
The Baltic

Abstract. In this paper, we estimate the surface water retention of nitrogen (N) in all the 117 drainage basins to the Baltic Sea with the use of a statistical model (MESAW) for source apportionment of riverine loads of pollutants. Our results show that the MESAW model was able to estimate the N load at the river mouth of 88 Baltic Sea rivers, for which we had observed data, with a sufficient degree of precision and accuracy. The estimated retention parameters were also statistically significant. Our results show that around 380 000 t of N are annually retained in surface waters draining to the Baltic Sea. The total annual riverine load from the 117 basins to the Baltic Sea was estimated at 570 000 t of N, giving a total surface water N retention of around 40%. In terms of absolute retention values, three major river basins account for 50% of the total retention in the 117 basins; i.e. around 104 000 t of N are retained in Neva, 55 000 t in Vistula and 32 000 t in Oder. The largest retention was found in river basins with a high percentage of lakes as indicated by a strong relationship between N retention (%) and share of lake area in the river drainage areas. For example in Göta älv, we estimated a total N retention of 72%, whereof 67% of the retention occurred in the lakes of that drainage area (Lake Vänern primarily). The obtained results will hopefully enable the Helsinki Commission (HELCOM) to refine the nutrient load targets in the Baltic Sea Action Plan (BSAP), as well as to better identify cost-efficient measures to reduce nutrient loadings to the Baltic Sea.

scholarly journals The analysis of the impact of small retention on water resources in the catchment/ Analiza oddziaływania małej retencji na zasoby wodne zlewni

2014 ◽  
Vol 23 (1) ◽  
pp. 41-51 ◽  
Author(s):  
Waldemar Mioduszewski ◽  
Erik P. Querner ◽  
Zbigniew Kowalewski
Keyword(s):  
Surface Water ◽  
Water Retention ◽  
River Basins ◽  
Simulation Modelling ◽  
Small River ◽  
Water Reservoirs ◽  
Small Water ◽  
River Valleys ◽  
The Impact ◽  
Surface And Groundwater

Abstract The aim of this study was to analyse the impact of selected small water retention measures on surface and groundwater level in river basins. The study was limited to the analysis of measures like small water reservoirs, restoration of bogs and reconstruction of drainage systems in the river valleys. A few study cases were described. Dutch SIMGRO numerical model describing the regional surface water and groundwater flow has been used for simulation modelling of different cases. The result of the study has shown that small retention measures are a good and effective method to increase the ability to retain water in the small river basins. Construction of small water reservoirs and weirs on ditches and creeks and restoration of drained bogs can limit the fast outflow of precipitation and melting water from the catchment. The study has proved that the small water retention measures can be helpful for flood protection and in decreasing of drought threats in small river basins.

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