Xinhua Ma

Prof. Dr. Xinhua Ma

orcid

Research Focus & Metrics

Academic Career Length

15Years (2012-Present)

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

Representative Publications

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6 November 2018 in Universe
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Journal Article
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Rita BernabeiRita Bernabei
Rita Bernabei
Pierluigi BelliPierluigi Belli
Pierluigi Belli
ABAndrea Bussolotti
Andrea Bussolotti
FCFabio Cappella
Fabio Cappella
Vincenzo CaraccioloVincenzo Caracciolo
Vincenzo Caracciolo
ZYZipiao Ye
Zipiao Ye
The first results obtained by the DAMA/LIBRA–phase2 experiment are presented. The data have been collected over six independent annual cycles corresponding to a total exposure of 1.13 ton × year, deep underground at the Gran Sasso National Laboratory. The DAMA/LIBRA–phase2 apparatus, about 250 kg highly radio-pure NaI(Tl), profits from a second generation high quantum efficiency photomultipliers and of new electronics with respect to DAMA/LIBRA–phase1. The improved experimental configuration has also allowed to lower the software energy threshold. The DAMA/LIBRA–phase2 data confirm the evidence of a signal that meets all the requirements of the model independent Dark Matter annual modulation signature, at 9.5 σ C.L. in the energy region (1–6) keV. In the energy region between 2 and 6 keV, where data are also available from DAMA/NaI and DAMA/LIBRA–phase1, the achieved C.L. for the full exposure (2.46 ton × year) is 12.9 σ .

5 June 2024 in Geomechanics and Geophysics for Geo-Energy and Geo-Resources
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GXGong Xun
Gong Xun
XMXinhua Ma
Xinhua Ma
YLYuyang LIU
Yuyang LIU
The complexity of hydraulic fracture network generation during the fracturing of shale reservoirs is a key indicator of the effectiveness of fracture stimulation. To obtain as large a reservoir stimulation volume as possible, this paper reviews articles on the study of hydraulic fracture propagation mechanism during hydraulic fracturing, analyses the factors affecting hydraulic fracture propagation, and classifies them into two categories: geological factors and engineering factors. In particular, the geological factors affecting hydraulic fracture propagation are classified into five categories: mineral composition of the shale, connections between mineral grains, defects in the shale, geostress, and temperature. Various influencing factors act together, resulting in the hydraulic fracture propagation path is difficult to predict. Therefore, this paper firstly explores the hydraulic fracture propagation pattern under the action of single geological factors and specifies its action mechanism; secondly, it also analyses the hydraulic fracture propagation pattern under the combined action of multiple geological factors and analyses its action mechanism. It is clear that relatively high brittle mineral content and temperature, low stress anisotropy and cementation strength, and a more developed natural fracture network are conducive to the generation of a complex fracture network. By analyzing the influence mechanism of single factors and multiple factors, the influence mechanism of geological factors on hydraulic fracture propagation is identified, guiding the optimal design of hydraulic fracturing.

5 April 2017 in Pure and Applied Geophysics
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YSYuri Stenkin
Yuri Stenkin
VAVictor Alekseenko
Victor Alekseenko
ZCZeyu Cai
Zeyu Cai
ZCZhen Cao
Zhen Cao
CCClaudio Cattaneo
Claudio Cattaneo
JZJing Zhao
Jing Zhao

20 July 2016 in The Astrophysical Journal
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YLYe Liu
Ye Liu
ZCZhen Cao
Zhen Cao
SCSongzhan Chen
Songzhan Chen
YCYang Chen
Yang Chen
SCShuwang Cui
Shuwang Cui
(C(On behalf of the LHAASO Collaboration)
(On behalf of the LHAASO Collaboration)
Supernova remnants (SNRs) are believed to be the most important acceleration sites for cosmic rays (CRs) below ∼1015 eV in the Galaxy. High-energy photons, either directly from the shocks of the SNRs or indirectly from the interaction between SNRs and the nearby clouds, are crucial probes for the CR acceleration. Big progresses on observations of SNRs have been achieved by space- and ground-based γ-ray facilities. However, whether γ-rays come from accelerated hadrons or not, as well as their connection with the CRs observed at Earth, remains in debate. Large High Altitude Air Shower Observatory (LHAASO), a next-generation experiment, is designed to survey the northern part of the very high energy γ-ray sky from ∼0.3 TeV to PeV with the sensitivity of ≲1% of the Crab Nebula flux. In this paper, we indicate that LHAASO will be dedicated to enlarging the γ-ray SNR samples and improving the spectral and morphological measurements. These measurements, especially at energies above 30 TeV, will be important for us to finally understand the CR acceleration in SNRs.

11 February 2018 in Energies
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Journal Article
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DZDeliang Zhang
Deliang Zhang
DYDai Yu
Dai Yu
XMXinhua Ma
Xinhua Ma
LZLiehui Zhang
Liehui Zhang
BZBing Zhong
Bing Zhong
ZTZhengwu Tao
Zhengwu Tao
This paper presents two representative models to analyze the flow dynamic of multi-scale porous medium in hydraulic fractured horizontal shale gas wells. In this work, considering the characteristic mechanisms (multi-scale porous space, desorption and diffusion), flow equations in shale are established. After that, two representative models (discrete fracture model and dual-porosity model) are tailored to our issues. Solved by the control-volume finite element method (CVFEM), influences of fracture network system on productivity in shale reservoirs are analyzed in detail. Based on the analysis, the effects can be summarized as follow: at the beginning of production, high conductivity fracture network means more free gas could be produced; at the later part of production, high conductive fracture network can form a large low pressure region, which can not only stimulate the desorption of adsorbed gas, but also reduce the flow resistance to the well. Finally, the sensitivities of characteristic parameters in shale are discussed.

22 October 2014 in Journal of Ocean University of China
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Journal Article
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XMXinhua Ma
Xinhua Ma
TZTianjiao Zhu
Tianjiao Zhu
QGQianqun Gu
Qianqun Gu
RXRui Xi
Rui Xi
WWWei Wang
Wei Wang
Dehai LiDehai Li
Dehai Li