Long-term (1980–2010) changes in cropland phosphorus budgets, use efficiency and legacy pools across townships in the Yongan watershed, eastern China

Abstract

Quantitative information on cropland phosphorus (P) flows at the township scale is critical for developing sustainable P management measures under the smallholder farming system. This study addressed changes in cropland soil surface P budgets (i.e., net of P inputs and crop outputs), use efficiencies (i.e., the ratio between crop P uptake and total P input) and legacy P pools across 21 townships in the Yongan watershed of eastern China in 1980-2010. For the entire watershed, total P input (>98% from synthetic fertilizer and farmyard manure), crop uptake and budgets per cropland area increased from 50.4, 17.3 and 33.1 kg P ha À1 yr À1 in 1980 to 74.6, 20.5 and 55.1 kg P ha À1 yr À1 in 1995, and then sharply declined to 39.6, 11.4 and 28.2 kg P ha À1 yr À1 in 2010, respectively. Estimated P use efficiency decreased from 34% in 1980 to 26% in 1999 before slightly increasing to 28% in 2010. Although the 21 townships had similar temporal variations over the 1980-2010 period, P budgets and use efficiency showed 2-3-fold spatial variability among townships within a given year. Spatio-temporal variations in the P budget and use efficiency were mainly related to changes in P fertilization rates and patterns (i.e., ratio of applied synthetic fertilizer P and farmyard manure P) and cropland types. The 20 townships having soil data had 87-720% and 113-395% increases of Olsen-P and total P contents in the upper 20 cm of cropland soils between 1984 and 2009, respectively. Increased soil TP level between 1984 and 2009 suggested that more than 53-79% of the cumulative P budget accumulated as legacy P pools in cropland soils. Based on regression analyses, legacy soil P contribution to annual crop P uptake was estimated to increase from 0.47 kg P ha À1 yr À1 (3%) in 1980 to 3.45 kg P ha À1 yr À1 (31%) in 2010, with 52-80% from synthetic fertilizer and 2-46% from farmyard manure. Improved utilization of soil legacy P pools for crop production and increasing P use efficiency are necessary to minimize P inputs and reduce nonpoint source P pollution load. The high spatial heterogeneity in P budgets and use efficiencies across townships, as well as considerable legacy soil P pools after long-term over-application, should be considered in developing P management strategies under smallholder farm systems.

Anthropogenic Phosphorus Inputs to a River Basin and Their Impacts on Phosphorus Fluxes Along Its Upstream‐Downstream Continuum

“…NAPI can be calculated as the sum of its major components, which include P fertilizer application, nonfood P and P in net food and feed imports (Hong et al, ). Evidence from Lake Erie (H. Han et al, ), the Baltic Sea (Hong et al, ), Lake Michigan (H. Han et al, ), and some watersheds in China (Chen, Hu, Guo, et al, ; Chen et al, ; Zhang, Swaney, Hong, et al, ) showed that NAPI has advantages not only in predicting riverine P fluxes but also in determining the extent of P accumulation and surplus (Y. Han et al, ), in assessing riverine P pollution (Chen, Hu, Guo, et al, ; H. Han et al, ; Russell et al, ), and in evaluating the pattern of P retention (Hong et al, ).…”

Legacy Nutrient Dynamics at the Watershed Scale: Principles, Modeling, and Implications

“…Changes in farm management, such as precision agricultural practices and inclusion of manure legume crops, could also enhance utilization of available inorganic and organic nutrients in soil (Haygarth et al, 2013). In some acidic soil regions, conversion of upland to paddy field management can improve bioavailability of legacy soil P as a result of flooding events (iron reduction and oxidation cycles, Chen et al, 2017). In many alkaline soil regions, decreasing soil pH through ammonium application can facilitate mobilization of P from calcium phosphates, leading to enhanced N and P uptake at early critical growth stages (Jing et al, 2010).…”

Influence of land use on the persistence effect of riverine phosphorus

“…Obviously, the legacy effect (or persistence effect) must be taken into account in watershed nutrient modelling efforts to fully inform watershed management activities. The few studies that have made efforts to quantify legacy P effects found that it is a very important component of riverine nutrient fluxes and that additional future research is necessary to better understand the mechanisms involved across a wide range of watershed conditions (Chen, Hu, Guo, et al, ; Chen, Hu, Wang, et al, ; Chen et al, ).…”