2019
DOI: 10.1016/j.agee.2018.11.015
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Spatio-temporal changes of cropland soil pH in a rapidly industrializing region in the Yangtze River Delta of China, 1980–2015

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Cited by 42 publications
(21 citation statements)
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“…It was worth noting that the relationships among the auxiliary variables are more likely to be spatially non‐stationary in this county. The possible reasons are as follows: (i) soil properties usually have strong spatial variability in large‐scale areas (Granger et al., 2017); (ii) soil properties are affected by multiple endogenous factors such as soil parent material and pedogenic processes, and the above endogenous factors are usually spatially non‐stationary in large‐scale areas (Qu, Chen, Huang, & Zhao, 2020; Zhao et al., 2010); (iii) soil properties in Shayang County are also strongly affected by exogenous factors such as land‐use patterns and fertilization, and the effects of the above exogenous factors on different soil properties also vary from place to place (Schleus et al., 1998; Xie et al., 2019). Therefore, the relationships among the soil properties were not constant in space, and PCA built on variable space could not effectively capture such non‐stationary relationships.…”
Section: Resultsmentioning
confidence: 99%
“…It was worth noting that the relationships among the auxiliary variables are more likely to be spatially non‐stationary in this county. The possible reasons are as follows: (i) soil properties usually have strong spatial variability in large‐scale areas (Granger et al., 2017); (ii) soil properties are affected by multiple endogenous factors such as soil parent material and pedogenic processes, and the above endogenous factors are usually spatially non‐stationary in large‐scale areas (Qu, Chen, Huang, & Zhao, 2020; Zhao et al., 2010); (iii) soil properties in Shayang County are also strongly affected by exogenous factors such as land‐use patterns and fertilization, and the effects of the above exogenous factors on different soil properties also vary from place to place (Schleus et al., 1998; Xie et al., 2019). Therefore, the relationships among the soil properties were not constant in space, and PCA built on variable space could not effectively capture such non‐stationary relationships.…”
Section: Resultsmentioning
confidence: 99%
“…However, although cropland SOC accumulation can be achieved through enhancing the C input (i.e., improving the straw/stover management), future SOC sequestration in the area is still facing big challenges, in particular the balance between agricultural development and the urbanization process for ensuring soil carbon input to maintain the SOC levels. A high SOC level not only benefits the biodiversity of agroecosystems (Wiesmeier et al, 2019), but also improves key soil functions, such as the capacity for acid buffering (Ritchie & Dolling, 1985), which are especially important for areas with accelerated soil acidification, e.g., this study area (Xie et al, 2019). Therefore, management practices and policies for enhancing the soil carbon input should still be given the top priority for maintaining the stability of SOC levels.…”
Section: Challenge For Soil Carbon Sequestrationmentioning
confidence: 99%
“…At pH ≤4.5, a large amount of soluble Al remains in soil solution with toxic Al 3+ as the dominant species (Kopittke & Blamey, 2016). In severe cases, soil acidification results in the deficiency of plant nutrients such as P, Mo, K, Ca, and Mg (Xie et al, 2019;Zhang et al, 2008).…”
Section: Introductionmentioning
confidence: 99%