Increasing maize production and preventing water deficits in semi-arid areas: A study matching fertilization with regional precipitation under mulch planting
Introduction
Maize (Zea mays L.) is an important cereal crop that is widely used as food for humans and livestock, as well as raw material for industrial production. In 2014, 2.2 × 108 ha of maize were planted around the world, yielding 1.2 × 1012 kg of grain (FAO, 2015). Global demand for maize grain is expected to double by 2050 due to population growth and the increasing demand for industrial raw materials (CIMMYT, 2011). To minimize the need for additional arable land, total grain production must be increased through intensification of productivity, that is, increasing crop yields per unit of cultivated land (Gu et al., 2019; Teixeira et al., 2014). However, maize production is increasingly at risk due to global climate change and unpredictability of precipitation patterns. Especially at high risk are the more than half of maize growing areas that are under dryland conditions (FAO, 2015). For example, maize yields are highly uncertain in semi-arid areas of the Loess Plateau, China, because of rare and uneven precipitation, as well as the use of unvalidated nutrition management practices.
The Loess Plateau (32–41 °N, 107–114 °E) in northwest China is a typical arid and semi-arid region where poverty is endemic. The Plateau comprises 341 counties, with a total area of 648,700 km2 and total cultivated land area of approximately 150,000 km2. Because of its lack of vegetation, loose soil, and large variation in precipitation (2–5 times difference between wet and dry years), this region has seriously eroded soil and is one of the most fragile ecological environments in the world (Deng et al., 2006; Li et al., 2009b). The average annual precipitation in this region is only about 460 mm, while the water surface evaporation capacity is up to 1500–2000 mm. Thus, groundwater and surface water available for farmland irrigation are scarce (Dong et al., 2019). The shortage of water resources is the most critical factor restricting the crop yields in the Loess Plateau region. In addition, 60 % of the annual precipitation in this region occurs from July to September (summer to autumn) in the form of heavy rains or rainstorms. As a result, spring droughts are common, which impedes seed germination and seedling growth and can lead to crop failures.
Researchers have been exploring efficient water use technologies for semi-arid areas (Gan et al., 2013; Chai et al., 2014), and showed that ridge-furrow construction combined with plastic film mulch planting is an efficient approach to dryland agriculture production. This practice consists of alternating ridges and furrows, with ridges covered in transparent plastic film (Mo et al., 2016; Zhang et al., 2019; Zhao et al., 2014). This technology improves the efficiency of rain collection by coupling ridge runoff and furrow precipitation, and creates an impermeable barrier to inhibit the loss of water and heat from the soil surface (Han et al., 2004; Wang et al., 2008). This significantly improves the hydrothermal environment of crops, promoting their growth and development and improving yields and resource utilization efficiency (Chai et al., 2014; Gan et al., 2013). At present, the two ridge-furrow mulching planting methods that have been studied and applied most often are ridge-furrow construction with full plastic film mulching (RFF, Fig. 1a) and ridge-furrow construction with half plastic film mulching (RFH, Fig. 1b) (Zhang et al., 2019; Zhao et al., 2014).
Fertilization contributes up to 40 % of crop yields, making this one of the most important agricultural production measures (Ju et al., 2009; Li et al., 2009a). Since the 1990s, China has become the largest consumer of fertilizers (i.e., nitrogen, phosphorus, potassium, and compound fertilizers) in the world, with total consumption increasing from 26 million tons in 1989 to about 60 million tons now. However, in many semi-arid areas, including the Loess Plateau, unvalidated nutrient (both excessive and insufficient) management, in addition to water availability, limits crop productivity (Bu et al., 2014; Li et al., 2009a; Liu et al., 2014). Within a certain range, fertilizers can promote crop growth and water use, but fertilization in excess of this range cannot significantly improve crop yields, disrupting a fragile water balance and introducing further uncertainty in agricultural production (Liu et al., 2014). Due to the extensive application of mulch planting, water and heat availability in some semi-arid areas, including the Loess Plateau, has changed (Bu et al., 2013; Liu et al., 2010). Therefore, matching fertilization management techniques with new water resource patterns in response to mulch planting is the key to ensure sustainable water use and crop productivity. Without this attention, agricultural water may be depleted and regional food security will continue to deteriorate.
Many studies have shown that soil water storage at sowing is an important parameter in agricultural production of dryland wheat (Li et al., 2004; Meng et al., 2012). Sufficient soil water can directly alleviate water stress to promote seed germination and emergence (Li et al., 2004; Meng et al., 2012), mitigate extreme changes in soil temperature to prevent crop damage from freezes (Liu et al., 2016), and promote dissolution and diffusion of nutrients to increase their availability(Li et al., 2009b). Each of these factors can help stimulate crop productivity and reduce the uncertainty associated with the amount of precipitation after sowing on the growth of wheat (Dong et al., 2019; Meng et al., 2012). However, current studies rarely focus on soil water at sowing with maize (especially under mulch planting) because maize growth is generally believed to coincide with the hydrothermal peak in summer. As patterns of agricultural hydrothermal resources change, studies on how to match fertilization amount with regional precipitation under high-efficiency ridge-furrow mulch planting is of vital importance to improve maize production in the Loess Plateau, as well as to ensure regional water and food security. The objectives of this study were to: 1) study the effects of fertilization and precipitation on soil water dynamics (especially at the time seeds are sown), maize yields, and water use efficiency (WUE) with common mulch planting methods; 2) clarify the effective strategy that matching fertilizer application with regional precipitation to achieve sustainable water use and crop productivity in semi-arid areas. 3) develop early warning schemes to prevent water deficit for maize production, and to compare the water use potential between RFF and RFH that the two typical mulching methods in semi-arid areas.
Section snippets
Experimental site
A field experiment was conducted in 2014–2017 at the experimental station for dry farming of Northwest A&F University, Pengyang County, Ningxia Hui Autonomous Region, China. The region is typical of the Loess Plateau—hilly with a warm temperate climate. In the past 40 years (1974–2014), the average annual temperature was about 7℃, annual precipitation was about 430 mm, sunshine duration was 2518 h, and frost-free period was 150–170 days. During the four years of the experiment (2014, 2015, 2016
Soil water storage (SWS)
Despite a dynamic change of increasing after decreasing as maize grew in each growing season, however, SWS at depths of 0–200 cm generally decreased with increasing fertilization during the four years, and moreover the decreasing trend gradually intensified over time across all fertilization treatments (Fig. 3). Under RFF planting, SWS changed from 575.5 mm at sowing in 2014 to 420.0–581.3 mm varied with the amount of fertilizer applied at maturity in 2017, whereas SWS changed from 575.5 mm to
Soil water
In ridge-furrow mulching systems, water circulation between the film and topsoil is improved. Water vapor forms and liquid drops condense under the film and gradually permeate the soil, which significantly improves soil moisture, especially at the soil surface (Gan et al., 2013; Wu et al., 2017). In the current study, compared with RFH, RFF decreased SWS to a certain extent from the jointing to silking stages of maize growth (Fig. 3). Perhaps the main reason was that RFF accelerated the growth
Conclusion
During this four-year study in the Loess Plateau, fertilization significantly promoted the absorption of soil water by maize adopting plastic film mulching and improved the dry matter accumulation, grain yields and water use efficiency of the maize. However, long-term fertilization, and especially long-term excess fertilization, can create a water imbalance, leading to a gradual decrease in soil water storage at sowing and a growing risk of maize production failure especially when precipitation
Declaration of Competing Interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgements
This work was supported by the National High-Tech Research and Development Program of China (“863 Program”) during the 12th 5-Year Plan (2013AA102902), the Chinese Special Fund for Agro-scientific Research in the Public Interest (201303104), and the Program of Introducing Talents of Discipline to Universities (B12007).
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