Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Modeling of asymmetric vertical growth in elogated hydraulic fractures and application to first MWX stimulation

Conference · · Soc. Pet. Eng. AIME, Pap.; (United States)
OSTI ID:6069808
When a continuous sand is bounded by zones of higher, but unequal, minimum in-situ stress, a vertically asymmetric hydraulic fracture results. The modeling is much more difficult than in the symmetric case mainly because the width equation is harder to formulate and solve. In this paper we present the principal components of the modeling, which includes non-Newtonian flow, leakoff with spurt loss, and ''storage'' of fluid due to volume expansion. The assumption is that the fracture is highly elongated, i.e., stress contrasts between pay and bounding zones are relatively large (> about few hundred psi). Vertical gradients of minimum in-situ stress and fluid pressure can be included in the modeling. To illustrate, the results, we present design calculations for a 30,000 gallon fracture, which was the first stimulation in the Multi-Well Experiment. The 80 ft fracture interval in the Paludal zone has at its upper edge a 520 psi stress contrast, and at its lower edge a 1195 psi contrast. Computed f
Research Organization:
Oral Roberts Univ.
OSTI ID:
6069808
Report Number(s):
CONF-8405120-
Conference Information:
Journal Name: Soc. Pet. Eng. AIME, Pap.; (United States) Journal Volume: SPE/DOE/GRI 12879
Country of Publication:
United States
Language:
English

Similar Records

Modeling of asymmetric vertical growth in elongated hydraulic fractures and application to first MWX (multi--well experiment) stimulation
Conference · Sat Dec 31 23:00:00 EST 1983 · Soc. Pet. Eng. AIME, Pap.; (United States) · OSTI ID:6194764

Numerical model of massive hydraulic fracture. Final report. [SYMFRAC1]
Technical Report · Thu Feb 28 23:00:00 EST 1985 · OSTI ID:6108263

Numerical model of massive hydraulic fracture. Second annual report, September 1981-August 1982
Technical Report · Fri Jul 01 00:00:00 EDT 1983 · OSTI ID:5947886