Pengcheng Luo

Prof. Pengcheng Luo

Shihezi University, Shihezi, Xinjiang, China
orcid

Research Focus & Metrics

Academic Career Length

4Years (2023-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

View All Publications
6 March 2024 in Soil and Tillage Research
Verified
Journal Article
Closed access
MTMingdong Tan
Mingdong Tan
WLWenhao Li
Wenhao Li
RZRui Zong
Rui Zong
XLXuanzhi Li
Xuanzhi Li
YHYue Han
Yue Han
Zhenhua WangZhenhua Wang
Zhenhua Wang

1 February 2023 in Water
Verified
Journal Article
Open access
PDF file
Dongwang WangDongwang Wang
Dongwang Wang
LZLiang Zhang
Liang Zhang
JZJinzhu Zhang
Jinzhu Zhang
WLWenhao Li
Wenhao Li
HLHaiqiang Li
Haiqiang Li
Zhenhua WangZhenhua Wang
Zhenhua Wang
Xinjiang is short on freshwater resources and rich in ones. The unregulated use of brackish water for agriculture leads to the aggravation of secondary salinization in soil; however, magnetization can improve the quality of brackish water. To evaluate the effects of magnetized brackish water drip irrigation on the water and salt transport characteristics of sandy soil in southern Xinjiang, China, a field plot experiment was carried out in which irrigation water was treated using one or two water magnetization events at different magnetization intensities. Water was treated at five magnetization intensities: 1000, 2000, 3000, 4000, or 5000 Gs, while unmagnetized water was used as the control. The results showed that the magnetization of brackish water used in drip irrigation decreased the water transport rate and increased the water holding capacity of the root layer soil. Magnetized irrigation water enhanced the leaching of soil salt and reduced the rate of salt accumulation. Compared with the control, the salt content of the magnetized water-irrigated soil decreased by 15.0%~33.7%, and the salt storage in the magnetized water-irrigated soil decreased by 44.99%~86.78%. The lowest rate of salt accumulation (4.96%) was observed at a magnetization intensity of 3000 Gs. Magnetized water irrigation changed the composition and proportions of soil ions, and Na+, Cl−, and SO42− leaching from the soil increased. The effect of magnetizing the irrigation water twice was greater than that of one magnetization event. Magnetizing the water twice at an intensity of 3000 Gs led to the largest decrease in the relative percentage contents of Na+ and Cl−, which were 80.90% and 82.36%, respectively. The magnetization intensity had a significant effect on the soil carbon and nitrogen contents, which showed a trend of first increasing and then decreasing as the magnetization intensity rose. The total carbon content after irrigation with magnetized water increased by 13.48%~63.35%, and the total nitrogen content increased by 11.73%~147.96%. The magnetization treatment of irrigation water can therefore reduce the risk of soil salinization and reduce salinity stress on crops in arid regions, providing a new method for alleviating the shortage of freshwater resources in Xinjiang and a means to use brackish water safely while improving salinized soil.

15 June 2024 in Agronomy
Verified
Journal Article
Open access
PDF file
YCYu Chen
Yu Chen
JZJinzhu Zhang
Jinzhu Zhang
Zhenhua WangZhenhua Wang
Zhenhua Wang
HLHaiqiang Li
Haiqiang Li
RCRui Chen
Rui Chen
Pengcheng LuoPengcheng Luo
Pengcheng Luo
Capillary water, serving as a crucial intermediary between groundwater and crop root layer moisture, is important for both soil retention and crop utilization. To investigate the effect of mulched drip irrigation (MDI) on upward capillary water in cotton fields with different application years (0, 10, 14, 18, 20, and 24 years) in the saline–sodic region of Northwest China, an indoor soil column test (one-dimensional capillary water rise experiment) was conducted. The results showed that the wetting front transport law, capillary water recharge, and wetting front transport rate over time exhibited an increasing trend in the early stages of MDI application (10 and 14 years), peaking at 18 years of application, followed by a decreasing trend. The relationship between the capillary water recharge and rising height was fitted based on the Green–Ampt model, and their slopes reveal that 14 and 18 years of MDI application required the largest amount of water per unit distance, indicating an excellent water-holding capacity beneficial for plant growth. Conversely, 0 years required the smallest amount of water per unit distance. Based on the movement characteristics of upper capillary water, we confirmed that the MDI application years (0–18 years) improves soil infiltration capacity, while the long-term application years (18–24 years) reduces groundwater replenishment to the soil. Furthermore, the HYDRUS-1D model was employed to simulate the capillary water rise process and soil moisture distribution under different MDl application years. The results showed an excellent consistency with the soil column experiments, confirming the accuracy of HYDRUS-1D in simulating the capillary water dynamics in saline–sodic areas. The results would provide suggestions to achieve the sustainable development of long-term drip-irrigated cotton fields.

25 April 2024 in Journal of the Science of Food and Agriculture
Verified
Journal Article
Closed access
Shudong LinShudong Lin
Shudong Lin
QWQuanjiu Wang
Quanjiu Wang
XZXue Zhao
Xue Zhao
YGYunna Gu
Yunna Gu
KWKai Wei
Kai Wei
MDMingjiang Deng
Mingjiang Deng

24 February 2025 in Soil and Tillage Research
Verified
Journal Article
Closed access
Pengcheng LuoPengcheng Luo
Pengcheng Luo
LZLu Zhao
Lu Zhao
RCRui Chen
Rui Chen
PCPengpeng Chen
Pengpeng Chen
YDYam Prasad Dhital
Yam Prasad Dhital
Zhenhua WangZhenhua Wang
Zhenhua Wang

16 May 2025 in Computers and Electronics in Agriculture
Verified
Journal Article
Closed access
QLQinggang Liu
Qinggang Liu
ZWZhenhua Wang
Zhenhua Wang
JZJinzhu Zhang
Jinzhu Zhang
NLNingning Liu
Ningning Liu
RCRui Chen
Rui Chen
Pengcheng LuoPengcheng Luo
Pengcheng Luo