System dynamics simulation of soil water resources with data support from the Yucheng Comprehensive Experimental Station, North China

System dynamics (SD) is one of the most suitable methods available to simulate and quantify the behaviour of complex systems due to it non-linear, multivariable, information feedback and temporally changing characteristics. This paper has improved on Khan et al.'s established model (see Khan et al. (2009) ‘Analyzing complex behavior of hydrological systems through a system dynamics approach’, Environmental Modeling & Software24, 1363–1372) by adding water production functions for three main crops (winter wheat, summer maize and cotton) based on soil water balance at the field level. Conclusions based on the simulation were as follows. (1) The model could simulate the dynamics of water balance components of winter wheat and summer maize relatively accurately through testing and validation. (2) Two to four irrigations were needed for the water-use requirement for winter wheat and summer maize when irrigation level was 75 mm each time. Cotton did not need to be irrigated except for the addition of 60 mm pre-sowing water. (3) Exploiting groundwater as far as possible and taking measures to reduce soil evaporation and at the same keeping irrigation unchanged was one of the best ways for sustainable utilization of water resources in the upper reaches of the Panzhuang District. (4) Water-use efficiencies were consistent with the regions' measured results showing that the model could simulate the water cycle in the field comparatively accurately.

Download Full-text

Water Resources in Chile

10.4018/978-1-7998-8482-8.ch007 ◽

2022 ◽

pp. 90-100

Author(s):

Javier Lozano Parra ◽

Jacinto Garrido Velarde ◽

Ignacio Aguirre

Keyword(s):

Water Resources ◽

Water Balance ◽

Greenhouse Gas ◽

Soil Water ◽

Water Availability ◽

Soil Water Balance ◽

Soil Water Availability ◽

Gas Concentration ◽

Spatially Distributed ◽

Soil Water Resources

This study quantifies the current and future soil water balance in a spatially distributed way for the whole of Chile and establishes what biomes will be the most affected by variations in water resources. The study of water resources reveals that 90% of surface Chile will reduce its soil water resources in the future if greenhouse gas concentration in the atmosphere does not stop. The most disadvantaged biomes are the forests, where soil water availability could decrease an average of 100 mm/year. Desert biomes could not perceive the hydrological imbalances; however, it is expected its surface increases.

Download Full-text

An Ammoniated Straw Incorporation Increased Biomass Production and Water Use Efficiency in an Annual Wheat-Maize Rotation System in Semi-Arid China

Agronomy ◽

10.3390/agronomy10020243 ◽

2020 ◽

Vol 10 (2) ◽

pp. 243 ◽

Cited By ~ 1

Author(s):

Yufeng Zou ◽

Hao Feng ◽

Shufang Wu ◽

Qin’ge Dong ◽

Kadambot H. M. Siddique

Keyword(s):

Winter Wheat ◽

Water Use Efficiency ◽

Soil Water ◽

Water Use ◽

Biomass Yield ◽

N Fertilizer ◽

Summer Maize ◽

Rotation System ◽

Use Efficiency ◽

Straw Incorporation

Water shortage and excessive chemical fertilizers application result in low soil water and nutrient availability and limit crop production in the Loess Plateau of Northwest China. Ammoniated straw incorporation with N fertilization may be an efficient strategy to maintain agricultural sustainability. However, the interactive effects of straw incorporation and N fertilizer on the biomass water use efficiency (WUE) in the winter wheat–summer maize rotation system remain unclear. A 3-year field experiment was conducted to evaluate the effects of combining ammoniated straw incorporation and N fertilizer on soil water, biomass yield and biomass water use efficiency (WUE) in an annual summer maize (Zea mays L.)—Winter wheat (Triticum aestivum L.) rotation system. There were three treatments: (i) long straw (5 cm) mulching with N fertilizer (CK), (ii) long straw with N fertilizer plowed into the soil (LP), and (iii) ammoniated long straw with N fertilizer plowed into the soil (ALP). Compared with the CK treatment, LP and ALP led to a similar soil water storage capacity. ALP improved summer maize biomass yield and winter wheat biomass yield at the jointing-maturity stage. ALP improved summer maize WUE at the ten-leaf collar-tasseling stage and winter wheat WUE from the tillering stage to the maturity stage. Also, the ALP treatment increased the total water use efficiency (TWUE) of winter wheat by 4.1–22.0%. Overall, ammoniated straw incorporation produced the most favorable biomass yield and WUE in the summer maize—Winter wheat rotation system in the Loess Plateau of China.

Download Full-text

Water use by winter wheat as affected by soil management

The Journal of Agricultural Science ◽

10.1017/s0021859600043458 ◽

1984 ◽

Vol 103 (1) ◽

pp. 189-199 ◽

Cited By ~ 11

Author(s):

M. J. Goss ◽

K. R. Howse ◽

Judith M. Vaughan-Williams ◽

M. A. Ward ◽

W. Jenkins

Keyword(s):

Winter Wheat ◽

Soil Water ◽

Water Deficit ◽

Water Use ◽

Management Practices ◽

Soil Management ◽

Maximum Depth ◽

Water Extraction ◽

Soil Water Deficit ◽

Potential Yield

SummaryIn each of the years from September 1977 to July 1982 winter wheat was grown on one or more of three clay soil sites (clay content 35–55%) in Oxfordshire where the climate is close to the average for the area of England growing winter cereals.The effects on crop water use of different soil management practices, including ploughing, direct drilling and subsoil drainage, are compared. Cultivation treatment had little effect on the maximum depth of water extraction, which on average in these clay soils was 1·54 m below the soil surface. Maximum soil water deficit was also little affected by cultivation; the maximum recorded value was 186±7·6 mm. Subsoil drainage increased the maximum depth of water extraction by approximately 15 cm and the maximum soil water deficit by about 17 mm.Generally soil management had little effect on either total water use by the crop which was found to be close to the potential evaporation estimated by the method of Penman, or water use efficiency which for these crops was about 52 kg/ha par mm water used.Results are discussed in relation to limitations to potential yield.

Download Full-text

Energy balance closure on a winter wheat stand: comparing the eddy covariance technique with the soil water balance method

Biogeosciences ◽

10.5194/bg-13-63-2016 ◽

2016 ◽

Vol 13 (1) ◽

pp. 63-75 ◽

Cited By ~ 19

Author(s):

K. Imukova ◽

J. Ingwersen ◽

M. Hevart ◽

T. Streck

Keyword(s):

Energy Balance ◽

Water Balance ◽

Winter Wheat ◽

Water Content ◽

Soil Water ◽

Water Storage ◽

Soil Water Balance ◽

Soil Water Storage ◽

Water Balance Method ◽

Closure Method

Abstract. The energy balance of eddy covariance (EC) flux data is typically not closed. The nature of the gap is usually not known, which hampers using EC data to parameterize and test models. In the present study we cross-checked the evapotranspiration data obtained with the EC method (ETEC) against ET rates measured with the soil water balance method (ETWB) at winter wheat stands in southwest Germany. During the growing seasons 2012 and 2013, we continuously measured, in a half-hourly resolution, latent heat (LE) and sensible (H) heat fluxes using the EC technique. Measured fluxes were adjusted with either the Bowen-ratio (BR), H or LE post-closure method. ETWB was estimated based on rainfall, seepage and soil water storage measurements. The soil water storage term was determined at sixteen locations within the footprint of an EC station, by measuring the soil water content down to a soil depth of 1.5 m. In the second year, the volumetric soil water content was additionally continuously measured in 15 min resolution in 10 cm intervals down to 90 cm depth with sixteen capacitance soil moisture sensors. During the 2012 growing season, the H post-closed LE flux data (ETEC =  3.4 ± 0.6 mm day−1) corresponded closest with the result of the WB method (3.3 ± 0.3 mm day−1). ETEC adjusted by the BR (4.1 ± 0.6 mm day−1) or LE (4.9 ± 0.9 mm day−1) post-closure method were higher than the ETWB by 24 and 48 %, respectively. In 2013, ETWB was in best agreement with ETEC adjusted with the H post-closure method during the periods with low amount of rain and seepage. During these periods the BR and LE post-closure methods overestimated ET by about 46 and 70 %, respectively. During a period with high and frequent rainfalls, ETWB was in-between ETEC adjusted by H and BR post-closure methods. We conclude that, at most observation periods on our site, LE is not a major component of the energy balance gap. Our results indicate that the energy balance gap is made up by other energy fluxes and unconsidered or biased energy storage terms.

Download Full-text

Variations of global and continental water balance components as impacted by climate forcing uncertainty and human water use

Hydrology and Earth System Sciences ◽

10.5194/hess-20-2877-2016 ◽

2016 ◽

Vol 20 (7) ◽

pp. 2877-2898 ◽

Cited By ~ 73

Author(s):

Hannes Müller Schmied ◽

Linda Adam ◽

Stephanie Eisner ◽

Gabriel Fink ◽

Martina Flörke ◽

...

Keyword(s):

Water Resources ◽

Water Balance ◽

Water Use ◽

Climate Forcing ◽

Land Area ◽

Water Balance Components ◽

Climate Forcings ◽

The Impact ◽

Global Water

Abstract. When assessing global water resources with hydrological models, it is essential to know about methodological uncertainties. The values of simulated water balance components may vary due to different spatial and temporal aggregations, reference periods, and applied climate forcings, as well as due to the consideration of human water use, or the lack thereof. We analyzed these variations over the period 1901–2010 by forcing the global hydrological model WaterGAP 2.2 (ISIMIP2a) with five state-of-the-art climate data sets, including a homogenized version of the concatenated WFD/WFDEI data set. Absolute values and temporal variations of global water balance components are strongly affected by the uncertainty in the climate forcing, and no temporal trends of the global water balance components are detected for the four homogeneous climate forcings considered (except for human water abstractions). The calibration of WaterGAP against observed long-term average river discharge Q significantly reduces the impact of climate forcing uncertainty on estimated Q and renewable water resources. For the homogeneous forcings, Q of the calibrated and non-calibrated regions of the globe varies by 1.6 and 18.5 %, respectively, for 1971–2000. On the continental scale, most differences for long-term average precipitation P and Q estimates occur in Africa and, due to snow undercatch of rain gauges, also in the data-rich continents Europe and North America. Variations of Q at the grid-cell scale are large, except in a few grid cells upstream and downstream of calibration stations, with an average variation of 37 and 74 % among the four homogeneous forcings in calibrated and non-calibrated regions, respectively. Considering only the forcings GSWP3 and WFDEI_hom, i.e., excluding the forcing without undercatch correction (PGFv2.1) and the one with a much lower shortwave downward radiation SWD than the others (WFD), Q variations are reduced to 16 and 31 % in calibrated and non-calibrated regions, respectively. These simulation results support the need for extended Q measurements and data sharing for better constraining global water balance assessments. Over the 20th century, the human footprint on natural water resources has become larger. For 11–18% of the global land area, the change of Q between 1941–1970 and 1971–2000 was driven more strongly by change of human water use including dam construction than by change in precipitation, while this was true for only 9–13 % of the land area from 1911–1940 to 1941–1970.

Download Full-text

Assessing water use and soil water balance of planted native tree species under strong water limitations in Northern Chile

New Forests ◽

10.1007/s11056-018-9689-6 ◽

2018 ◽

Vol 49 (6) ◽

pp. 871-892 ◽

Cited By ~ 2

Author(s):

Horacio E. Bown ◽

Juan Pablo Fuentes ◽

Amanda M. Martínez

Keyword(s):

Water Balance ◽

Soil Water ◽

Water Use ◽

Tree Species ◽

Soil Water Balance ◽

Northern Chile ◽

Native Tree ◽

Native Tree Species ◽

Water Limitations

Download Full-text

High-Throughput Phenotyping of Crop Water Use Efficiency via Multispectral Drone Imagery and a Daily Soil Water Balance Model

Remote Sensing ◽

10.3390/rs10111682 ◽

2018 ◽

Vol 10 (11) ◽

pp. 1682 ◽

Cited By ~ 13

Author(s):

Kelly Thorp ◽

Alison Thompson ◽

Sara Harders ◽

Andrew French ◽

Richard Ward

Keyword(s):

Water Balance ◽

Water Use Efficiency ◽

Soil Water ◽

Water Use ◽

High Throughput ◽

Soil Water Balance ◽

Balance Model ◽

Crop Water ◽

Crop Water Use ◽

Use Efficiency

Improvement of crop water use efficiency (CWUE), defined as crop yield per volume of water used, is an important goal for both crop management and breeding. While many technologies have been developed for measuring crop water use in crop management studies, rarely have these techniques been applied at the scale of breeding plots. The objective was to develop a high-throughput methodology for quantifying water use in a cotton breeding trial at Maricopa, AZ, USA in 2016 and 2017, using evapotranspiration (ET) measurements from a co-located irrigation management trial to evaluate the approach. Approximately weekly overflights with an unmanned aerial system provided multispectral imagery from which plot-level fractional vegetation cover ( f c ) was computed. The f c data were used to drive a daily ET-based soil water balance model for seasonal crop water use quantification. A mixed model statistical analysis demonstrated that differences in ET and CWUE could be discriminated among eight cotton varieties ( p < 0 . 05 ), which were sown at two planting dates and managed with four irrigation levels. The results permitted breeders to identify cotton varieties with more favorable water use characteristics and higher CWUE, indicating that the methodology could become a useful tool for breeding selection.

Download Full-text

Double-Double Row Planting Mode at Deficit Irrigation Regime Increases Winter Wheat Yield and Water Use Efficiency in North China Plain

Agronomy ◽

10.3390/agronomy10091315 ◽

2020 ◽

Vol 10 (9) ◽

pp. 1315

Author(s):

Xun Bo Zhou ◽

Guo Yun Wang ◽

Li Yang ◽

Hai Yan Wu

Keyword(s):

Winter Wheat ◽

Soil Water ◽

Water Use ◽

Deficit Irrigation ◽

Water Status ◽

Row Spacing ◽

Soil Water Depletion ◽

Double Row ◽

Water Depletion ◽

Use Efficiency

Low water availability coupled with poor planting method has posed a great challenge to winter wheat (Triticum aestivum L.) productivity. To improve productivity and water use efficiency (WUE) under deficit irrigation, an effective water-saving technology that is characterized by three planting modes has been developed (uniform with 30-cm row spacing (U), double-double row spacing of 5 cm (DD), and furrow-ridge row spacing of alternated 20 cm and 40 cm (F)) combined with three irrigation regimes (50 mm water each at growth stage 34 (GS34) and GS48 (W1), and 100 mm water at GS48 (W2), or 100 mm each water at GS34 and GS48 (W3)). Results showed that DD increased yield by 9.7% and WUE by 12.6% due to higher soil water status and less soil water depletion and evapotranspiration compared with U. Although the soil water status, soil water depletion, evapotranspiration, and yield increased with increasing irrigation amount, more soil water depletion and evapotranspiration resulted in low WUE. The deficit irrigation was beneficial for improving WUE as W1 had significantly increased yield by 5.4% and WUE by 7.1% compared with W2. Yield and evapotranspiration showed a quadratic dynamic equation indicating that yield increased with increasing evapotranspiration. Considering WUE and relatively higher yield under deficit water, W1 combined with DD is suggested to be a good management strategy to be applied in winter wheat of water-scarce regions.

Download Full-text