Shale bedding planes control rock removal behaviors of PDC cutter: Single cutter experiment

Shale bedding planes control rock removal behaviors of PDC cutter: Single cutter experiment

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Journal Pre-proof Shale bedding planes control rock removal behaviors of PDC cutter: Single cutter experiment Mao Sheng, Zhen Cheng, Shuyang Gao, Huaizhong Shi, Yanlong Zhang PII:

S0920-4105(19)31061-7

DOI:

https://doi.org/10.1016/j.petrol.2019.106640

Reference:

PETROL 106640

To appear in:

Journal of Petroleum Science and Engineering

Received Date: 12 June 2019 Revised Date:

19 September 2019

Accepted Date: 31 October 2019

Please cite this article as: Sheng, M., Cheng, Z., Gao, S., Shi, H., Zhang, Y., Shale bedding planes control rock removal behaviors of PDC cutter: Single cutter experiment, Journal of Petroleum Science and Engineering (2019), doi: https://doi.org/10.1016/j.petrol.2019.106640. This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. Please note that, during the production process, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. © 2019 Published by Elsevier B.V.

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Shale bedding planes control rock removal behaviors of PDC cutter: single

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cutter experiment

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Mao Shenga,b*, Zhen Chenga,b, Shuyang Gaoc, Huaizhong Shia,b, Yanlong Zhangd

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a. State Key Laboratory of Petroleum Resources and Prospecting, (China University of Petroleum-Beijing), Beijing 102249, P.R. China

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b. College of Petroleum Engineering, China University of Petroleum-Beijing, 102249, P.R. China

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c. Sinopec Research Institute of Petroleum Engineering, Beijing, 10010, P.R. China

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d. CNPC Engineering Technology R&D Company Limited, Beijing, 102200, China

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* Correspondence to: Mao Sheng, E-mail: [email protected]

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The highlight of this work can be presented as:

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1) A parabolic correlation was observed between cutting force and bedding inclination.

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2) Shear cracking along the weak bedding planes promotes chipping.

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3) Bedding inclination controls the rock removal behaviors from crushing-dominate to

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chipping-dominate.

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Abstract

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Shale bedding planes arise with the complexity of rock removal by the PDC cutters. A series of single

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cutter experiments were conducted to understand the effects of bedding planes of shale on chip

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formation behaviors. Six bedding inclinations were taken into account by recording the variation of

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cutting force, cutting size, topography of debris, and high-speed images. Results demonstrate that the

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average cutting force highly correlates with bedding inclination where a parabolic relation is observed.

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The maximum value of cutting force is presented while perpendicular cutting to the bedding plane.

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Crushing and chipping are approved to be two mechanisms of rock removal of the laminated shale.

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Particularly, the bedding plane controls the chip formation behaviors. While the cutting force is

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perpendicular to shale bedding, the crushing dominates the rock removal process in which more powder

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debris are created. While the cutting force is parallel to shale bedding, the chipping dominates the rock

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removal and more chunk-like cuttings are generated. Shear cracking along the weak bedding planes

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promotes chipping that is controlled by the bedding inclination. In summary, the bedding plane

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attributes to the variation of cutting force response, cutting size distribution, and even rock removal

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mechanisms.

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Keywords: shale, PDC, bedding plane, rock failure, chip formation

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1 Introduction

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Efficient drilling of Polycrystalline Diamond Compact (PDC) bit in shale formation recently attracts

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much more attention since it is widely applicable in horizontal well drilling (Hanna, Douglas et al. 2011,

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Soeder 2018, Zhai, Wang et al. 2018). Bedding plane is one nature of shale formation where the weak

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strength and anisotropy mechanical properties fully exist. Figure 1 illustrates the contact relation of

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PDC cutters and bedding planes with a contact angle. The contact angle would result in a more

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complex shale drilling process. In order to offer basic guidelines for PDC cutter design and efficiency

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improvement, influences of bedding planes on cutting force response and drilling efficiency should be

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well recognized.

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Fig. 1 Diagram of PDC bit drilling in bedding shale formation

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Crushing and chipping are two widely accepted mechanisms of rock removal of the fixed cutters.

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The crushing mode creates highly fractured and inelastically deformed rock, while major cracks initiate

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and propagate to form big chips in chipping mode (Mishnaevsky 1995). However, the crushing and

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chipping of rock is an extremely complex failure and cracking process that is controlled by two aspects:

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rock properties and cutting situation. Cheatham and Daniels (Cheatham and Daniels 1979) investigated

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the bit balling problems of clay shale drilling through single cutter experiments at atmospheric and

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hydrostatic pressure conditions. They found that, the ductile and sticky nature of the clay shale were 3

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two major contributors to the problems that the chip formation was similar to that of ductile metals

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cutting. However, the cuttings generated under hydrostatic pressure were observed to be almost

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identical to those achieved by cutting lead at atmospheric pressure. Finger (Finger 1984) developed a

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linear cutting testbed and conducted a systematical rock cutting experiment on Berea sandstone and

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Westerly granite. The large chips and a crushed powdery zone were identified by fluorescent dye. The

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observations from experimental works were validated by Finite element and Discrete element

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simulation (Huang, Detournay et al. 1999, Rojek, Onate et al. 2011, Jaime, Zhou et al. 2015). The

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crushing failure and shear cracking mechanics were clarified through numerical analysis. Recently, Che

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et al. (Che, Zhang et al. 2017) (Che and Ehmann 2014) proposed a comprehensive experimental scheme

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to measure the force response and visualize chip formation process on Indiana limestone, Austin chalk,

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and Berea sandstone. The chipping mode was found to highly correlate with the depth of cut, the rake

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angle, and the rock types. Furthermore, they proposed a new cutting model by accounting for the

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crushing zone and crack propagation behaviors from the observations of linear rock cutting (Che, Zhu

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et al. 2016). The alternate sudden movements during chip formation was captured by high-speed

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imaging and the crushing mode was found to occupy most of the time of an entire crushing and

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chipping cycle (Cheng, Sheng et al. 2018). Moreover, the rake angle of the PDC cutter dramatically

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affects the removal behaviors of crushed material where different cutting faces corresponds to specific

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frictional angle and shear force on the rock failure plane. (Yahiaoui, Paris et al. 2016, Rostamsowlat,

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Richard et al. 2018) Although the rock removal mechanisms have been illuminated so far from

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numerical simulation and visualization experiments, yet most of studied rocks are relatively isotropic

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and homogenous. The impacts of rock anisotropy, particularly weak bedding planes, are still required to

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be recognized.

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Many investigations attributed the anisotropy of rock mechanics and special failure behaviors to the

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bedding planes of shale (Chenevert and Gatlin 1965, McLamore and Gray 1967, Niandou, Shao et al.

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1997, Heng, Guo et al. 2015, Chen, Lan et al. 2018). The orientations of bedding planes determined the

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failure mode since the weak strength is along the bedding planes. Moreover, the bedding plane slip was

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identified to present a significant effect on borehole and casing stability. Special breakout patterns of the

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laminated shale failure were found to be different from that of the isotropic formation and were

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controlled by bedding inclination and in-situ stress conditions (Tien, Kuo et al. 2006, Labiouse and

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Vietor 2014, Meier, Rybacki et al. 2015). Additionally, hydraulic fracture propagation was also

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confirmed to be affected by bedding planes which promote the complexity of fracture network (Yushi,

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Xinfang et al. 2016, Lin, He et al. 2017, Tang, Wu et al. 2018). In aspects of rock cutting, Ozcelik and

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Yilmazkaya (Ozcelik and Yilmazkaya 2011) found the rock anisotropy, particularly the bedding

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inclination to the cutting direction, was naturally sensitive to the cutting efficiency and force response

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of diamond wire cutting. Gong and Liu (Gong, Zhao et al. 2005) (Liu, Xu et al. 2019) proposed a 2D

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TBM cutting model to illustrate the joint orientation. They found the joint orientation could influence

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the crack initiation and propagation as well as the fragmentation pattern. Though tremendous studies

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demonstrate the importance of bedding planes on rock failure, wellbore stability, and hydraulic fracture

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propagation, yet most of those studies did not discuss the effects of bedding plane on rock removal

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mechanisms of PDC cutters, particularly for the cutting force response, chip formation process, and

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complicated mechanisms.

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In this paper, a series of single cutter experiments on laminated shale was conducted by considering

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a wide range of bedding inclinations from 0° to 150°. The dynamic responses of cutting force, cutter

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acceleration, and debris size distribution were obtained at different bedding inclinations. Extraordinary

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crushing and chipping patterns were captured by high-speed imaging technique. Based on the observed

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phenomena, a conceptual cutting model of laminated shale formation was proposed and further

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mechanisms were discussed.

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2 Materials and method

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2.1 Linear rock cutting testbed

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A linear rock cutting testbed was built based on a mechanical shaping machine as illustrated in Figure 2.

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The testbed could precisely control the cutting speed (100~1200mm/min) and cutting depth (accuracy

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of 0.01 mm). A cutter holder was particularly designed to fix single PDC cutter. The rake angle of cutter

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was capable to adjust into five levels of negative 15, 20, 25, 30, 35, 40 degrees. A planar PDC cutter

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with diameter of 13 mm and thickness of 25 mm, as a typical PDC bit cutter, was selected for this study.

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The rock block was fixed by a specific holder to limit X and Y direction movement. In order to achieve

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a linear cutting, the rock block was fed toward the cutter in x-direction while the cutter was kept

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stationary.

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Most importantly, the testbed was well equipped with a force measuring system, including a

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single-component strain gauge (KYOWA KFWB-5-120-C1), which is close to the PDC cutter, a

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unidirectional accelerator fixed at the cutter holder, and a data acquisition unit with a maximum

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sampling rate of 100 Hz. Besides, a high-speed camera (Phantom V310) was used to visualize the chip

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formation. The maximum resolution and recording speed of this high-speed camera are 1280 × 1024

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and 50,000 fps.

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Figure 2 Schematic diagram of (a) linear cutting testbed, (b)single PDC cutter scratching on shale block, and (c) Conceptual model of single PDC cutting on bedding shale 119

2.2 Rock specimen preparation

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Organic-rich shale is our target material where these samples were collected from the outcrop of Lower

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Silurian Longmaxi formation, which is located at south Sichuan basin in Changning, China. The

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bedding plane is well rich in the Longmaxi Shale as shown in Figure 3. Mineralogical composition was

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obtained from X-ray diffraction as listed in Table 1 and it can be seen that over 60% minerals belong to

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brittle minerals. Particularly, the clay minerals mainly consist of illite without serious hydration

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swelling problems. The mechanical properties were particularly measured in different bedding

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inclinations, according to ISRM standard.

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The specimens were cored from the same block and reshaped into the cubic blocks with side length of

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200 mm by using a diamond-saw cutting machine. Fine polish was carried out to ensure the parallelism

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of opposite surfaces of specimen was less than 100 µm. The sample can be reused after milling and

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polishing cutting surface again. In total, six cubic blocks were prepared with six bedding inclinations of

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0o, 30o, 60o, 90o, 120o, and 150o (Figure 3). The specimen was required to be dried in an oven at 100

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for 48 hours before testing in order to remove the fluid influence.

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Figure 3 Photographs of six cubic blocks with the bedding inclinations of 0o, 30o, 60o, 90o, 120o,

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and 150o

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Table 1. Mineral components and content of shale sample Minerals

Weight content (wt.%)

Quartz

22.2~35.1%

Clay

14.5~19.2%

Calcite

26.8~31.4%

Feldspar

1.2~2.6%

Pyrite

1.1~3.1%

Siderite

0.2~0.4%

Dolomite

11.6~30.2%

Total

100%

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Table 2 Rock mechanical properties of shale sample Bedding inclination (°)

Rock density (g/cm3)

Young’s modulus (GPa)

Poisson ratio (1)

UCS (MPa)

36.04

0.145

189.65

30.74

0.153

107.96

60

36.54

0.131

79.66

90

42.15

0.231

142.25

0 30 2.53~2.59

8

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2.3 Experimental design and procedures

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A series of linear rock cutting tests were conducted on the cubic shale blocks. The variable parameter of

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the experiment was bedding inclination. Except that, other cutting parameters including the cutting

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depth, cutting speed, and rake angle were controlled as constant. Before each test, the PDC cutter was

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first moved vertically to set a prescribing cutting depth at the edge of the specimen. Then the rock was

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fed toward the cutter along horizontal direction at a given cutting speed. For each test, the horizontal

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force and acceleration on the cutter holder, regarding as horizontal cutting force, were recorded through

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a uniaxial strain gauge and accelerator with a sampling rate of 100 Hz. A high-speed camera captured

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the chip formation process in the sample rate of 1000 frame per second. After test, the rock debris were

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collected by brush clean and the sieve analysis was carried out to obtain five groups of size: 0/10mesh,

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10/20mesh, 20/40mesh, 40/80mesh, and 80/

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obtained to indicate the debris size distribution. The scratch profiles were finally imaged by 3D Laser

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profile instrument and electrical microscope. In order to ensure the experimental repeatability, there are

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three repeated tests in this study.

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2.4 Force signal processing

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Since the force and accelerator sensors were mounted on the cutter holder and kept stationary, there was

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no signal while the stage moves without cutting. When the stage started to move at a constant cutting

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speed, the PDC cutter will apply a cutting force on the shale sample. Meanwhile, system vibration and

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discontinuously crushing and chipping process also led to dynamic acceleration change of the cutter.

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The undesired noise originated from the system vibration usually belongs to a low frequency signal.

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Hence, the low pass filter was used to ensure the noise-free force responses. The dynamic force

mesh. The weight percentage of each group was finally

9

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responses that expose a strong oscillation with respect to time indeed reflect sufficient information on

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the rock removal behaviors, such as crushing and chipping phenomenon. Unfortunately, the dynamic

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force responses are difficult to be characterized in a simple way. Previous researchers proposed the use

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of average force within a certain cutting distance or period of time and then study the change of the

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average forces with respect to various process parameters. In this study, both average cutting force and

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frequency analysis were used to identify the influences of bedding plane on rock removal mechanisms.

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3. Results

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3.1 Influence of shale bedding on cutting force responses

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Force responses, as important indicator of the rock cutting processes, are capable of revealing the

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intrinsic mechanisms of rock cutting in a quantitative way. As shown in Figure 4, continuous force data

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indicates a fairly periodic fluctuation in a certain amplitude and frequency. The force response can be

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divided into two groups according to the amplitude and frequency of cutting force. Firstly, a relatively

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big amplitude but low frequency force was observed from the specimens with bedding inclinations of

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0°, 30°, 120°, 150°. Secondly, a low amplitude but high frequency force is obvious for bedding

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inclinations of 60°, 90°. Moreover, the macro and micro cracks were observed from the bottom and

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edge of scratch profiles. Discontinuously crushing and chipping occurs at shale rock cutting inferred

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from the fluctuation of cutting force and rough scratch surfaces.

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Figure 4. Responses of horizontal cutting force of single PDC cutter on shale bedding

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As shown in Figure 5, a strong correlation can be observed between the time-averaged force

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responses and bedding inclination. It behaves a parabolic curve in which the cutting force achieves

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maximum value of 3.15 KN at 90-degree orientation. Furthermore, the maximum force value at 90

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degree is more than twice value of the minimum force at 0 degree. It is interested that the cutting force

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at 120-degree orientation is only less than 60% cutting force at 60-degree orientation, though those two

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orientations are angle complementarity. However, there exists little difference between the cutting

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forces at 150-degree and 30-degree.

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Figure 5 Average horizontal cutting force versus bedding angle

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Figure 6 shows the time-dependent acceleration of PDC cutter when cutting through parallel or

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perpendicular to the shale beddings and their probability density distributions. A phenomenon was

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observed that the amount of strong acceleration while cutting perpendicular to the bedding plane was

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almost twice of that while cutting parallel to the bedding plane. It can be inferred that the vibration

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response of PDC cutter is highly related to the bedding inclination.

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Figure 6 Response of accelerate of single PDC cutter on parallel and vertical bedding

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3.2 Chip formation phenomena

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Chip formation is a process of rock debris creating controlled by the rock removal mechanisms. As

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shown in Figure 7, the chip formation process was observed when cutting perpendicular to the bedding

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plane. The powder cuttings are initially created in the front of PDC cutter and following several

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chunk-like cuttings ejected from shale matrix subsequently, which corresponds to the crushing and

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chipping phenomena, respectively.

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Figure 7 Chip formation process of single PDC cutter at the laminated shale, the parallel lines

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denote the bedding inclination.

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Chip formation photography of different bedding inclinations were compared as illustrated in Figure 8.

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Both the crack propagation and the final shape of chips dramatically change with the bedding

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inclination. For instance, the wedge-plate cuttings were present while cutting parallel to the bedding

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plane, but the slim-rod cuttings appeared in perpendicular cutting.

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Figure 8 Chipping phenomenon for different bedding inclinations, the parallel lines denote the

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bedding inclination

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The cutting size distributions and their photography at different bedding inclinations were plotted

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in Figure 9. It can be seen that the weight percentages of the fine debris (more than 20 mesh) perform a

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good agreement with the cutting force response to the bedding inclination. If cutting perpendicular to

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the bedding plane, more fine debris and less chunk-like debris will be formed when compared with

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other orientations. However, the amount of chunk-like debris would be increasing when the cutting

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direction is parallel to the bedding plane.

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Figure 9 (a) Cutting size distribution and (b) photography for different bedding inclinations

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The topography of debris was reconstructed by 3D confocal microscope as shown in Figure 10.

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The topography changes from wedge plate to slim rod with the increasing bedding inclination.

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Moreover, the obvious shear planes can be found due to the results of shear failure from weak bedding

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planes. In other words, the weak bedding planes change the trajectory of shearing cracking.

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Figure 10 Photography and 3D laser profiles of cuttings for three typical bedding inclinations

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4 Discussion

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4.1 Bedding planes control chip formation behaviors

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Our results confirm that the bedding plane performs a profound influence on chip formation in the shale

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cutting process with a PDC cutter. There coexists powder and chunk-like cuttings from chip formation

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process. Moreover, the occurrence of periodic fluctuation of cutting force causes from two reasons: the

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increase of cutting force as the chip-boundary crack propagates through the rock ahead of the cutter,

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and then decrease as the chip detaches and the cutter moves into the vacant space. Such observations

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support that the crushing and chipping should be two primary rock removal mechanisms of laminated

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shale. Particularly, the bedding inclination determines the domination of crushing and chipping in the

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rock removal. More chunk-like cuttings produced indicates that the chipping dominates rock removal

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when cutting parallel to the bedding plane. More powder cuttings created demonstrates the chipping

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dominates rock removal when cutting perpendicular to bedding plane. The cutting force responses

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consist of these two processes; the crushing-dominated removal which consumes more cutting force

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while the chipping-dominated removal which consumes less. For practical drilling, it can be inferred

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that the efficiency of parallel drilling to the bedding plane is lower than that of perpendicular drilling.

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4.2 Mechanical influence of shale bedding on rock removal

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The variations of average cutting force originate from the mechanical influence of shale bedding. As

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illustrated in Figure 11, a conceptual model of PDC cutting on the laminated shale was proposed to

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demonstrate the force loading on the bedding planes. With a decrease of bedding inclination, an

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increase of shear force and decrease of normal force promotes shear crack generation, which is induced

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from weak bedding planes. Consequently, more chunk-like cuttings would be produced at low bedding

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inclination. However, with an increase of bedding inclination, it becomes harder for shear cracks to

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initiate because of the increase of normal stress on the bedding plane. In this situation, the PDC cutter

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should overcome the shear strength of rock matrix. Such mechanical analysis explains the cutting force

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perpendicular to the bedding plane is almost twice of that while parallel cutting.

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Figure 11 Conceptual model of PDC cutting on bedding shale with the rake angle of PDC cutter, α

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and bedding inclination, θ. Horizontal cutting force can be decomposed into normal force and 16

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shear force aligning with bedding plane.

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5 Conclusions

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Influences of bedding planes on rock removal behaviors were emphasized through a series of single

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cutter experiments. A wide range of bedding inclinations from 0° to 150° were taken account. It can be

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concluded that the bedding planes control the chip formation process of PDC cutter. The bedding plane

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attributes to the variation of cutting force response, cutting size distribution, and even rock removal

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mechanisms. Our observations support that the crushing and chipping are still two primary rock

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removal mechanisms of laminated shale. The bedding inclination regulates which mechanism

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dominates the rock removal behaviors. Finally, a mechanical model of PDC cutting which takes the

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bedding planes into consideration was proposed to clarify the impacts of bedding planes on rock

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fragmentation.

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Acknowledgements

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This work was financially supported by the National Natural Science Foundation of China (Grant

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No.U1562212) and the PetroChina Innovation Foundation (Grant No. 2018D-5007-0308).

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